The Arctic Coastal Dynamics Database: A New Classification Scheme and Statistics on Arctic Permafrost Coastlines

被引:0
作者
Hugues Lantuit
Pier Paul Overduin
Nicole Couture
Sebastian Wetterich
Felix Aré
David Atkinson
Jerry Brown
Georgy Cherkashov
Dmitry Drozdov
Donald Lawrence Forbes
Allison Graves-Gaylord
Mikhail Grigoriev
Hans-Wolfgang Hubberten
James Jordan
Torre Jorgenson
Rune Strand Ødegård
Stanislav Ogorodov
Wayne H. Pollard
Volker Rachold
Sergey Sedenko
Steve Solomon
Frits Steenhuisen
Irina Streletskaya
Alexander Vasiliev
机构
[1] Alfred Wegener Institute for Polar and Marine Research,Northern Canada Division
[2] Research Section Potsdam,Arctic Centre
[3] International Permafrost Association,undefined
[4] Geological Survey of Canada,undefined
[5] St. Petersburg State University,undefined
[6] International Arctic Research Center,undefined
[7] VNIIOkeangeologia,undefined
[8] Earth Cryosphere Institute,undefined
[9] RAS,undefined
[10] Geological Survey of Canada,undefined
[11] Nunatech Technologies,undefined
[12] Melnikov Permafrost Institute,undefined
[13] Antioch University New England,undefined
[14] ABR Inc,undefined
[15] Gjovik College,undefined
[16] Moscow State University,undefined
[17] McGill University,undefined
[18] International Arctic Science Committee,undefined
[19] University of Groningen,undefined
来源
Estuaries and Coasts | 2012年 / 35卷
关键词
Arctic; Coast; Permafrost; Erosion; Carbon cycle;
D O I
暂无
中图分类号
学科分类号
摘要
Arctic permafrost coasts are sensitive to changing climate. The lengthening open water season and the increasing open water area are likely to induce greater erosion and threaten community and industry infrastructure as well as dramatically change nutrient pathways in the near-shore zone. The shallow, mediterranean Arctic Ocean is likely to be strongly affected by changes in currently poorly observed arctic coastal dynamics. We present a geomorphological classification scheme for the arctic coast, with 101,447 km of coastline in 1,315 segments. The average rate of erosion for the arctic coast is 0.5 m  year−1 with high local and regional variability. Highest rates are observed in the Laptev, East Siberian, and Beaufort Seas. Strong spatial variability in associated database bluff height, ground carbon and ice content, and coastline movement highlights the need to estimate the relative importance of shifting coastal fluxes to the Arctic Ocean at multiple spatial scales.
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页码:383 / 400
页数:17
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