Acceleration of thaw slump activity in glaciated landscapes of the Western Canadian Arctic

Climate change is increasing the frequency and intensity of thermokarst, but the influences of regional climate and physiography remain poorly understood. Retrogressive thaw slumping is one of the most dynamic forms of thermokarst and affects many areas of glaciated terrain across northwestern Canad...

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Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Rebecca A Segal, Trevor C Lantz, Steven V Kokelj
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2016
Subjects:
Q
Ice
Online Access:https://doi.org/10.1088/1748-9326/11/3/034025
https://doaj.org/article/5225ceb0f2a045e6a2f14230efb52613