Shorelines of the Central Beaufort Sea, Alaska coastal region (Hulahula River to the Colville River) used in shoreline change analysis

• Main Authors: Gibbs, Ann E., Ohman, Karin A., Coppersmith, Ryan, Richmond, Bruce M.
• Format: Dataset
• Language: unknown
• Published: USGS Science Data Catalog 2017
• Subjects: Shoreline; Shoreline Change; Digital Shoreline Analysis System; DSAS; U.S. Geological Survey; USGS; Coastal and Marine Geology Program; CMGP; Pacific Coastal and Marine Science Center; PCMSC; National Assessment of Shoreline Change Project; National Assessment of Coastal Change Hazards; oceans; environment; geoscientificInformation; coastal processes; Habitat; shoreline accretion; shoreline erosion; North Slope; Beaufort Sea; Staines River; Sagavanirktok River; Colville River; Kuparuk River; Harrison Bay; Prudhoe Bay; Arctic National Wildlife Refuge; Canning River; State of Alaska; United States of America; Arctic; ANWR; Pacific; north slope; Alaska
• Online Access: https://search.dataone.org/view/e4eb9dde-ff90-4b66-b7c5-6a7d6941758c

This dataset includes shorelines from 63 years ranging from 1947 to 2010 for the north coast of Alaska between the Hulahula River and the Colville River. Shorelines were compiled from topographic survey sheets (T-sheets; National Oceanic and Atmospheric Administration (NOAA)), aerial orthophotographs (U.S. Geological Survey (USGS), National Aeronautics and Space Administration (NASA), Conoco-Philips (CP), British Petroleum Alaska (BPXA)), satellite imagery (State of Alaska), and lidar elevation data (USGS). Historical shoreline positions serve as easily understood features that can be used to describe the movement of beaches through time. These data are used to calculate rates of shoreline change for the U.S. Geological Survey's National Assessment of Shoreline Change Project. Rates of long-term and short-term shoreline change were generated in a GIS using the Digital Shoreline Analysis System (DSAS) version 4.3. DSAS uses a measurement baseline method to calculate rate-of-change statistics. Transects are cast from the reference baseline to intersect each shoreline, establishing measurement points used to calculate shoreline change rates.