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Recent Increases in Permafrost Thaw Rates and Areal Loss of Palsas in the Western Northwest Territories, Canada
Author(s) -
Mamet Steven D.,
Chun Kwok P.,
Kershaw Geoffrey G. L.,
Loranty Michael M.,
Peter Kershaw G.
Publication year - 2017
Publication title -
permafrost and periglacial processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.867
H-Index - 76
eISSN - 1099-1530
pISSN - 1045-6740
DOI - 10.1002/ppp.1951
Subject(s) - permafrost , active layer , physical geography , geology , altitude (triangle) , climate change , peat , vegetation (pathology) , climatology , archaeology , geography , oceanography , layer (electronics) , medicine , chemistry , geometry , mathematics , organic chemistry , pathology , thin film transistor
Decay of palsas can indicate permafrost status, particularly in regions where air temperatures have increased rapidly in recent decades. Using weather data, annual surveys of active‐layer thickness, and analyses of high‐resolution aerial imagery from the eastern Selwyn/western Mackenzie Mountains, NT, Canada, we show that permafrost temperatures have increased, active layers have deepened, and palsa areal extents have decreased considerably since the 1940s. High‐altitude palsas thawed quickly from the 1940s to the 1980s, although some low‐altitude palsas have recently decreased rapidly in areal extent due to peat‐block calving. The linear rate of increasing active‐layer thickness may not be congruent with the non‐linear rate of areal loss of palsas. The rapid and episodic collapse of palsas at some sites highlights the necessity to consider hydrology, vegetation cover, landscape position, and morphology in palsa dynamics in addition to a warming climate. Copyright © 2017 John Wiley & Sons, Ltd.