Coastal Change since 1950 in the Southeast Chukchi Sea, Alaska, Based on GIS and Field Measurements.

Manley WF, Mason OK, Jordan JW, Sanzone DM, Parrish EG, Lestak LR. 2007. Coastal Change since 1950 in the Southeast Chukchi Sea, Alaska, Based on GIS and Field Measurements.. National Park Service

Coastal environments at high latitudes are experiencing rapid change. Coastal erosion threatens a variety of near shore marine, terrestrial, and freshwater habitats, and may be accelerating with Arctic warming. To better understand impacts for national parks in northwestern Alaska, a collaborative study has begun to document coastal change in the southeast Chukchi Sea. A field-based component includes: repeat photography; mapping and description of sediments and landforms; and periodic ground-truth measurements of shoreline change since 1987 at 27 coastal monitoring sites. A geospatial component began with creation of digital orthoimagery over a large area (>6000 km2) at high resolution (1.0 m or better) for three "time slices": approx. 1950, approx. 1980, and 2003. Spatial analysis of bluff retreat was then conducted for selected areas near the monitoring sites using the USGS DSAS extension to ArcGIS. Results indicate that the GIS-based measurements have acceptably low errors (+/- 0.1 m/yr or better). Transects with 20-m spacing reveal high spatial variability related to coastal morphologies and processes. A comparison of the two time intervals suggests temporal variability also. For example, bluff erosion rates appear to have decreased after 1980 for the north-facing coast of Bering Land Bridge National Park while increasing after 1980 for the west-facing coast of Cape Krusenstern National Monument. In general, most of the >600-km-long coast from Wales to Kivalina has experienced erosion in the past five decades, with long-term average rates of 0 to -3 m/yr. Direct impacts include beach and bluff retreat, overwash deposition, migration or closure of inlets and lagoons, capture of thaw-lake basins, and release of sediment and organic carbon to nearshore waters. Higher temporal resolution is needed, but the coastal ecosystems in the region appear to be sensitive to: the frequency and intensity of storm events, increasing temperatures, permafrost melting, sea-level rise, and increasing length of the summer ice-free season. Arctic Coastal Zones at Risk, Scientific Workshop on the Impact of Global Climate Change on the Arctic Coastal Zones, Tromsø, Norway, Oct. 2007: http://coast.gkss.de/events/arctic07/

Type
Generic Document
Authors
Manley, William; Mason, Owen; Jordan, James; Sanzone, Diane; Parrish, Eric; Lestak, Leanne
Date of Issue
2007
Publisher
National Park Service
Units
BELA , CAKR

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