Thaw Subsidence in Undisturbed Tundra Landscapes, Barrow, Alaska, 1962-2015

Author:

Streletskiy Dmitry A.1,Shiklomanov Nikolay I.1,Little Jonathon D.2,Nelson Frederick E.34,Brown Jerry5,Nyland Kelsey E.3,Klene Anna E.6

Affiliation:

1. Department of Geography; The George Washington University; Washington DC USA

2. Monroe Community College; Rochester NY USA

3. Department of Geography; Michigan State University; East Lansing MI USA

4. Department of Earth, Environmental and Geographical Sciences; Northern Michigan University; Marquette MI USA

5. Falmouth MA USA

6. Department of Geography; University of Montana; Missoula MT USA

Funder

US National Science Foundation (NSF)

NSF and NASA under NSF Cooperative Agreement

Publisher

Wiley

Subject

Earth-Surface Processes

Reference38 articles.

1. Characteristics and significance of the transition zone in drained thaw lake basins of the Arctic Coastal Plain, Alaska;Bockheim;Arctic,2005

2. Some results of geothermal investigations of permafrost in northern Alaska;Brewer;Transactions, American Geophysical Union,1958

3. Soil properties developed on the complex tundra relief of northern Alaska;Brown;Builetyn Peryglacjalny,1969

4. Brown J Johnson PL 1965 Pedo-ecological investigations, Barrow, Alaska CRREL Technical Report

5. Brown J Johnson PL 1966 U.S. Army CRREL Topographic Map, Barrow, Alaska (1:25,000) U S Army CRREL Special Report

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