The coastal vulnerability index (C.V.I.) provides insight into the relative potential of coastal change due to future sea-level rise. The maps and data presented here can be viewed in at least two ways:
As ranked in this study, coastal geomorphology and coastal slope are the most important variables in determining the CVI. Wave height, relative sea-level rise, and tide range provide large-scale variability to the coastal vulnerability index. Erosion and accretion rates, where complete, contribute the greatest variability to the C.V.I. at short spatial scales. The rates of shoreline change, however, are the most complex and poorly documented variable in this data set. Most of the rates used here are based on a dated, low-resolution data set, and thus far, corrections have been made only on a preliminary level. To best understand where physical changes may occur, large-scale variables must be clearly and accurately mapped and small-scale variables must be understood on a scale that takes into account their geologic and environmental influences.