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Coastal Vulnerability Assessment of Cape Cod National Seashore to Sea-Level Rise, USGS Open-File Report 02-233

Map of Coastal Vulnerability

Skip past contents informationTable of Contents link to Title Page Link to Abstract Page Link to Introduction Page Link to Data Ranking Page Link to Cape Cod National Seashore Page Link to Methology Page Link to Geologic Variables Page Lilnk to Physical Process Variables Page Link to Calculating the Vulnerability Index Page Link to Results Page Link to Discussion Page Link to Conclusions Page Link to References Page

METHODOLOGY

In order to develop a GIS database for a park-wide assessment of coastal vulnerability, data for each of the six variables described above were gathered from state and federal agencies (Table 2). The database is based on that used by Thieler and Hammar-Klose (1999) and loosely follows an earlier database developed by Gornitz and White (1992). A comparable assessment of the sensitivity of the Canadian coast to sea-level rise is presented by Shaw et al. (1998).

The database was constructed using a 1:70,000 Cape Cod shoreline that was produced from the medium resolution digital vector U.S. shoreline provided by the Strategic Environmental Assessments (SEA) Division of NOAA's Office of Ocean Resources Conservation and Assessment (ORCA) (http://seaserver.nos.noaa.gov
/projects/shoreline/shoreline.html). Data for each of the six variables (geomorphology, shoreline change, coastal slope, relative sea-level rise, significant wave height, and tidal range) were joined to the shoreline using a 1 minute (approximately 1.5 km) grid (Figure 2). The data were next assigned a relative vulnerability value from 1-5 (1 is very low vulnerability, 5 is very high vulnerability) based on the potential magnitude of its contribution to physical changes on the coast as sea level rises (Table 1).

Figure 2. Shoreline grid for CACO.Click on figure for larger image.

Figure 2. Data for six variables (geomorphology, shoreline change, coastal slope, relative sea-level rise, significant wave height, and tidal range) were joined to the shoreline using a 1 minute grid

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