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

In some regions underlain by ice‐rich permafrost, a consistent, long‐term increase in ALT under changing climatic conditions is not supported by observations. The apparent lack of ALT may be attributed to soil consolidation from thawing of the uppermost ice‐rich permafrost and subsidence of the grou...

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Veröffentlicht in:	Permafrost and periglacial processes 2017-07, Vol.28 (3), p.566-572
Hauptverfasser:	Streletskiy, Dmitry A., Shiklomanov, Nikolay I., Little, Jonathon D., Nelson, Frederick E., Brown, Jerry, Nyland, Kelsey E., Klene, Anna E.
Format:	Artikel
Sprache:	eng
Schlagworte:	active layer Alaska Annual variations Barrow Climatic conditions Consolidation Elevation Frost frost heave Frost heaving Heaving Ice Ice wedges Interannual variability Landscape Permafrost Snow Snow depth Soil Soils Stability Subsidence Technology Technology utilization thaw subsidence Thawing Tundra Variability
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