Name: The long-term (plus additional erosion from a 100-yr storm) in 2010 with existing conditions (2010 water level) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2030 with medium sea level rise (93 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2050 with medium sea level rise (93 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2100 with medium sea level rise (93 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2030 with high sea level rise (167 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2050 with high sea level rise (167 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2100 with high sea level rise (167 cm by 2100) that considers existing coastal armoring
Name: The long-term (plus additional erosion from a 100-yr storm) in 2080 with extreme sea level rise (167 cm at 2080 only) that considers existing coastal armoring
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"tide_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion Current Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion Current Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion Current Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2030 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2060 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Cliff Erosion 2100 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) a safety buffer to account for along-shore variability in erosion rates (an indicator of extreme erosion events/block failures). The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climatestormier – Increased storminess (doubling of storm intensity in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 High Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 High Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 High Long Term Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion Current Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Low Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 High Long Term Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion Current Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Low Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 High Long Term and Large Storm No Change
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion Current Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Low Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Low Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Low Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 High Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 High Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 High Long Term and Large Storm Stop Mining
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion Current Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Low Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 Medium Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2030 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2060 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Dune Erosion 2100 High Long Term and Large Storm Doubling of El Niño
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ future erosion scenario +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Future erosion scenarios:nochange – A continuation of existing wave climate and sand miningstopmining – Stop sand mining (only applies to southern Monterey Bay)stormier – Increased storminess (doubling of El Niño storm impacts in a decade)-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave overtopping (waves running up over the beach and flowing into low-lying areas, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. This hazard zone also takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected to ocean over topography” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Monterey Bay Sea Level Rise Vulnerability Study. For detailed documentation about how these hazard zones were developed, please see "Monterey Bay Sea Level Rise Vulnerability Assessment: Technical Methods Report," a report prepared by ESA PWA for The Monterey Bay Sanctuary Foundation in March 2014.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (41 cm by 2100)s2 – Medium sea level rise (88 cm by 2100)s3 – High sea level rise (159 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Copyright Text: Environmental Science Associates - Philip Williams Associates, Ltd. (ESA PWA), 2014
Name: Tidal Inundation Combined 2030 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Tidal Inundation Combined 2060 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Tidal Inundation Combined 2100 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Tidal Inundation Current with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2030 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2060 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2100 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2030 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2060 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2100 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2030 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2060 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation 2100 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of Extreme Monthly High Water (EMHW, inundated once per month on average) tide inundation zones for all sea level rise scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Name: Tidal Inundation (monthly in meters) Current
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2030 Low
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2060 Low
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2100 Low
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2030 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2060 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2100 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2030 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2060 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Tidal Inundation (monthly in meters) 2100 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: These zones represent monthly tide inundation depths (areas that would be flooded by normal tides once per month, on average) for areas that are clearly connected to the ocean over topography. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_d" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent monthly tide inundation areas (areas that would be flooded by normal tides once per month, on average). The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month. These zones do not, however, consider coastal erosion or wave overtopping, which may change the extent and depth of regular tidal flooding in the future. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each rising tides dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"emhw_area" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Combined 2030 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Combined 2060 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Combined 2100 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Current with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2030 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2060 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2100 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2030 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2060 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2100 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2030 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2060 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term 2100 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure Current with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2030 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2060 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2100 Low with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2030 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2060 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2100 Medium with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2030 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2060 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Long Term Block Failure 2100 High with coastal armoring
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: This polygon represents the spatial aggregation of cliff erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of cliff erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of cliff erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion Current Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2030 Low Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2060 Low Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2100 Low Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2030 Medium Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2060 Medium Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2100 Medium Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2030 High Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2060 High Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Cliff Erosion 2100 High Long Term Block Failure
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent cliff erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “erosion hazard zones with buffer”) an additional buffer corresponding to an average block failure width was added on top of long term erosion distances. The inland extent of the hazard zones represent projections of the potential future cliff edge for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"chz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm or block failure.wbuffer - Includes long-term erosion and the locally determined potential block failure width (failure of the cliff hillslope, common erosion mechanism in Santa Barbara County).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Combined 2030 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Dune Erosion Combined 2060 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Dune Erosion Combined 2100 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Dune Erosion Long Term Current with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2030 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2060 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2100 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2030 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2060 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2100 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2030 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2060 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term 2100 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm Current with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2030 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2060 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2100 Low with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2030 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2060 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2100 Medium with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2030 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2060 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Long Term and Large Storm 2100 High with coastal armoring
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. These zones also consider the effect of existing coastal armoring structures. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of dune erosion hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion Current Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2030 Low Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2060 Low Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2100 Low Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2030 Medium Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2060 Medium Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2100 Medium Long Term and Large Storm
Display Field: Id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2030 High Long Term and Large Storm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2060 High Long Term and Large Storm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Dune Erosion 2100 High Long Term and Large Storm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These zones represent future dune (sandy beach) erosion hazard zones, incorporating site-specific historic trends in erosion, additional erosion caused by accelerating sea level rise, and (in the case of the “storm erosion hazard zones”) the potential erosion impact of a large storm wave event. The inland extent of the hazard zones represent projections of the potential future crest of the dunes for a given sea level rise scenario, planning horizon, and erosion scenario. Not all areas within the hazard zone are expected to erode to this extent by the specified planning horizon, but any location has the potential to erode to this extent for the selected scenario. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for Santa Barbara County in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"dhz" + _ + erosion projection type +_+ sea level rise scenario + planning horizon-------------------------------Erosion projection type:longterm - A continuation of historic erosion with additional erosion caused by sea level rise. Does not include potential impacts of a large storm.wstorm - Includes long-term erosion and the potential erosion of a large storm event (e.g. 100-year storm).-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm Combined 2030 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Flood Inundation by Large Storm Combined 2060 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Flood Inundation by Large Storm Combined 2100 with coastal armoring
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.
Name: Flood Inundation by Large Storm Current with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2030 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2060 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2100 Low with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2030 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2060 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2100 Medium with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2030 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2060 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2100 High with coastal armoring
Display Field: Connection
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015, as well as “Santa Barbara County Coastal Resiliency Phase 2 Coastal Hazard Modeling: Technical Methods Memorandum,” a report prepared by ESA for the County of Santa Barbara in July 2016.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Name: Flood Inundation by Large Storm 2030 Combined
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Name: Flood Inundation by Large Storm 2060 Combined
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Name: Flood Inundation by Large Storm 2100 Combined
Display Field: Year
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the spatial aggregation of coastal flooding hazard zones along the Santa Barbara County coastline for all sea level rise scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict flooding caused by a coastal storm. The processes considered include (1) storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), (2) wave run-up (waves running up the beach and over coastal property, calculated using the maximum historical wave conditions), (3) extreme lagoon water levels which can occur when lagoon mouths are closed and fill up during rainfall events, and (4) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider upland fluvial (river) flooding and local rain/run-off drainage, which likely play a large part in coastal flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. This difference is captured in the “Connection” attribute (either “connected” or “connectivity uncertain”) in each dataset. We recommend these be mapped as separate colors. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this shapefile reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"coastal_floodhz" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: This polygon represents the spatial aggregation of fluvial flooding hazard zones on Carpinteria Creek for all sea level rise scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of fluvial flooding hazard zones on Carpinteria Creek for all sea level rise scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: This polygon represents the spatial aggregation of fluvial flooding hazard zones on Carpinteria Creek for all sea level rise scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios (as reported in the “Num_Scen” attribute) that are projected to be inundated at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all scenarios and which areas may only hazardous for the worst case scenarios.-------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: These hazard zones depict the depth of fluvial flooding on Carpinteria Creek. The processes considered include (1) existing and future streamflow from climate change projections, and (2) additional flooding caused by rising sea level in the future. These hazard zones do NOT consider storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm), which could play a part in fluvial flooding, especially around coastal confluences where the creeks meet the ocean. There are two types of inundation areas: (1) areas that are clearly connected over the existing digital elevation through low topography, (2) and other low-lying areas that don’t have an apparent connection to the creek channel, as indicated by the digital elevation model, but are low-lying and flood prone from groundwater levels and any connections (culverts, underpasses) that are not captured by the digital elevation model. These apparently disconnected flood areas were left in due to the uncertainty of 1D fluvial models and potential for increased flooding from the coastal boundary, but were not attributed seperately. -------------------------------This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment. For detailed documentation about how these hazard zones were developed, please see "Santa Barbara County Coastal Hazard Modeling and Vulnerability Assessment: Technical Methods Report," a report prepared by ESA for The County of Santa Barbara in June 2015.-------------------------------The name of this raster reflects the future scenarios and planning horizon that the hazard zone represents, as follows:"fluvial_dep" + _ + sea level rise scenario + planning horizon-------------------------------Sea level rise scenarios:ec – Existing conditions (2010 water level)s1 – Low sea level rise (27 cm by 2100)s2 – Medium sea level rise (78 cm by 2100)s3 – High sea level rise (153 cm by 2100)-------------------------------Planning horizons:2010 (Existing conditions)203020602100
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for existing conditions (no sea level rise, 2010 water level) in 2010. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_ec2010.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for low sea level rise (1.44 feet by 2100, relative to 2010) in 2030. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s12030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for low sea level rise (1.44 feet by 2100, relative to 2010) in 2060. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s12060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) low sea level rise (1.44 feet by 2100, relative to 2010) in 2100. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s12100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2030 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) medium sea level rise (3 feet by 2100, relative to 2010) in 2030. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2060 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for medium sea level rise (3 feet by 2100, relative to 2010) in 2060. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2100 Medium
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for medium sea level rise (3 feet by 2100, relative to 2010) in 2100. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2030 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for high sea level rise (4.8 feet by 2100, relative to 2010) in 2030. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2060 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for high sea level rise (4.8 feet by 2100, relative to 2010) in 2060. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Tidal Inundation (monthly in feet) 2100 High
Display Field:
Type: Raster Layer
Geometry Type: null
Description: This raster represents the potential depth of inundation caused simply by rising tide levels (not considering storms, erosion, or river discharge) for high sea level rise (4.8 feet by 2100, relative to 2010) in 2100. The water level mapped in these inundation areas is the Extreme Monthly High Water (EMHW) level, which is a high water level that is reached approximately once a month (sea level rise added to the existing EMHW of 2.0 meters NAVD88). As sea level rises, the area of inundation will grow and water levels in already-inundated areas will deepen.This raster is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_depth_s32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w02030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w02060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w02100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 Medium Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w02030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 Medium Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w02060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 Medium Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the "continuation of existing wave climate" scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w02100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 High Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “continuation of existing wave climate” scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w02030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 High Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “continuation of existing wave climate” scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w02060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 High Existing Wave Climate
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “continuation of existing wave climate” scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w02100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 Low Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 Low Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 Low Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 Medium Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 Medium Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 Medium Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 High Doubling of El Niño Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 High Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 High Doubling of El Nino Frequency
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño frequency” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the low sea level rise scenario (44 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s1w32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2030 Medium Addition of ARkStorm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2060 Medium Addition of ARkStorm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: Erosion Risk 2100 Medium Addition of ARkStorm
Display Field: scen
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the coastal erosion hazard zone for the medium sea level rise (93 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s2w32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2030 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2060 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal erosion hazard zone for the high sea level rise (148 cm by 2100, relative to 2010) and the “doubling of El Niño Frequency and Arkstorm in the year 2060” wave scenario at the 2100 planning horizon. The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_erosionHZ_s3w32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for existing conditions (no sea level rise, 2010 water level) in 2010. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_ec2010.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for low sea level rise (44 cm by 2100, relative to 2010) in 2030. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s12030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for low sea level rise (44 cm by 2100, relative to 2010) in 2060. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s12060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for low sea level rise (44 cm by 2100, relative to 2010) in 2100. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s12100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for medium sea level rise (93 cm by 2100, relative to 2010) in 2030. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for medium sea level rise (93 cm by 2100, relative to 2010) in 2060. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for medium sea level rise (93 cm by 2100, relative to 2010) in 2100. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for high sea level rise (148 cm by 2100, relative to 2010) in 2030. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for high sea level rise (148 cm by 2100, relative to 2010) in 2060. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the potential extent of flooding caused by coastal processes during a large coastal storm wave event for high sea level rise (148 cm by 2100, relative to 2010) in 2100. The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. Two components of coastal flooding are incorporated in this hazard area: flooding caused by storm waves rushing inland and flooding due to ocean storm characteristics such as storm surge (a rise in the ocean water level caused by waves and pressure changes during a storm). This hazard zone takes into account areas that are projected to erode in the future, sometimes leading to additional flooding through new hydraulic connections between the ocean and low-lying areas. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_combine_storm_floodHZ_s32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for existing conditions (no sea level rise, 2010 water level) in 2010. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_ec2010.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for low sea level rise (44 cm by 2100, relative to 2010) in 2030. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s12030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for low sea level rise (44 cm by 2100, relative to 2010) in 2060. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s12060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for low sea level rise (44 cm by 2100, relative to 2010) in 2100. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s12100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for medium sea level rise (93 cm by 2100, relative to 2010) in 2030. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for medium sea level rise (93 cm by 2100, relative to 2010) in 2060. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for medium sea level rise (93 cm by 2100, relative to 2010) in 2100. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for high sea level rise (148 cm by 2100, relative to 2010) in 2030. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s32030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for high sea level rise (148 cm by 2100, relative to 2010) in 2060. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s32060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the coastal storm wave impact area for high sea level rise (148 cm by 2100, relative to 2010) in 2100. The coastal storm wave impact area is one component of the overall coastal storm flood hazard zone. This hazard area is somewhat analogous to the FEMA V-zone, where the dominant hazard is wave momentum. This is the zone where water is projected to rush inland due to waves breaking at the coast and can damage structures, move cars, and knock people off their feet.The coastal storm flood hazard zones were developed using representative wave conditions based on observed historical events, with added sea level rise. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_coastal_storm_waveHZ_s32100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) Current
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the existing conditions 100-year floodplains for the Santa Clara and Ventura Rivers, at existing conditions (no sea level rise, 2010 water level).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_ec2010.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2030 Medium
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2030, assuming the B1 future emissions scenario and medium sea level rise (93 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s2B12030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2060 Medium
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2060, assuming the B1 future emissions scenario and medium sea level rise (93 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s2B12060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2100 Medium
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2100, assuming the B1 future emissions scenario and medium sea level rise (93 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s2B12100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2030 High
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2030, assuming the A2 future emissions scenario and high sea level rise (148 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s3A22030.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2060 High
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2060, assuming the A2 future emissions scenario and high sea level rise (148 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s3A22060.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Name: River Flood Inundation (large storm) 2100 High
Display Field: id
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: This polygon represents the projected 100-year floodplains for the Santa Clara and Ventura Rivers in 2100, assuming the A2 future emissions scenario and high sea level rise (148 cm by 2100, relative to 2010).This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
<a href='xml/ventura_river100-yr_floodplain_s3A22100.xml'target='_blank'><b>Metadata</b><a></br>
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the spatial aggregation of coastal erosion hazard zones for all sea level rise and wave climate scenarios at the 2030 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios that are projected to be hazardous at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise and wave scenarios and which areas may only hazardous for the worst case scenarios.The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the spatial aggregation of coastal erosion hazard zones for all sea level rise and wave climate scenarios at the 2060 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios that are projected to be hazardous at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise and wave scenarios and which areas may only hazardous for the worst case scenarios.The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the spatial aggregation of coastal erosion hazard zones for all sea level rise and wave climate scenarios at the 2100 planning horizon. At each planning horizon, the hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios that are projected to be hazardous at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise and wave scenarios and which areas may only hazardous for the worst case scenarios.The coastal erosion hazard zones incorporate three components of potential future erosion: a historic trend in erosion, additional erosion caused by sea level rise, and the potential erosion impact of a large storm wave event. The planning horizons were selected based on guidance from the Coastal Resilience Ventura steering committee.This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the number of future scenarios projecting storm-induced flooding for the 2030 planning horizon. At each planning horizon, the combined storm flood hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios projected to cause flooding at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise scenarios and which areas may only be hazardous for the worst case scenarios, for a given planning horizon.These hazard areas combine the coastal erosion, fluvial storm flooding, wave impact area, and coastal storm flood hazard zones into a single, comprehensive, combined storm flood hazard area. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the number of future scenarios projecting storm-induced flooding for the 2060 planning horizon. At each planning horizon, the combined storm flood hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios projected to cause flooding at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise scenarios and which areas may only be hazardous for the worst case scenarios, for a given planning horizon.These hazard areas combine the coastal erosion, fluvial storm flooding, wave impact area, and coastal storm flood hazard zones into a single, comprehensive, combined storm flood hazard area. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy
Description: This polygon represents the number of future scenarios projecting storm-induced flooding for the 2100 planning horizon. At each planning horizon, the combined storm flood hazard zones for all scenarios are overlaid into a single “spatially aggregated” layer that counts the number of scenarios projected to cause flooding at a particular location. This is intended to be a planning tool that helps identify which areas will be hazardous for all sea level rise scenarios and which areas may only be hazardous for the worst case scenarios, for a given planning horizon.These hazard areas combine the coastal erosion, fluvial storm flooding, wave impact area, and coastal storm flood hazard zones into a single, comprehensive, combined storm flood hazard area. This feature is one in a series of coastal flood and erosion hazard zones developed as part of the Coastal Resilience Ventura project. For detailed documentation about how these hazard zones were developed please see "Coastal Resilience Ventura: Technical Report for Coastal Hazards Mapping," a report prepared by ESA PWA for The Nature Conservancy.
Copyright Text: Environmental Science Associates - Philip Williams and Associates (ESA PWA), San Francisco and The Nature Conservancy