COASTAL GEOMORPHOLOGICAL VECTORS OF CHANGE: APPLICATION OF MONITORING PROTOCOLS IN PARKS AND REFUGES
One-dimensional shoreline position is recorded seasonally using mapping-grade GPS units with sub-meter accuracy; the resulting datasets are analyzed within a GIS to determine zones of positive or negative displacement. Within each site, a series of two-dimensional beach-dune profiles show a network of elevational cross-sections. This network is analyzed within the context of the entire system to determine trends of sediment flow alongshore, identify areas of erosion and/or deposition, and establish how specific geomorphological features are evolving. Three-dimensional digital elevation models (DEMs) of the entire beach-dune system are constructed for areas of special interest. These DEMs are compared temporally to derive the volume of sediment within a system, how it changes seasonally, and how it responds to disturbance events such as major storms. The GPS equipment used to collect the 2-D and 3-D data is survey-grade, accurate to within centimeters.
These metrics are presented in annual and long-term trend reports that provide critical information on the geotemporal evolution of coastal systems. Currently, these protocols are utilized within 19 National Wildlife Refuges, 4 National Parks, and 1 National Estuarine Research Reserve. Additionally, the GIS datasets resulting from these efforts are maintained in a national geodatabase.