Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks

<p>The intensification of thaw-driven mass wasting is transforming glacially conditioned permafrost terrain, coupling slopes with aquatic systems, and triggering a cascade of downstream effects. Within the context of recent, rapidly evolving climate controls on the geomorphology of permafrost...

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Bibliographic Details
Main Authors: S. V. Kokelj, J. Kokoszka, J. van der Sluijs, A. C. A. Rudy, J. Tunnicliffe, S. Shakil, S. E. Tank, S. Zolkos
Format: Article
Language:English
Published: Copernicus Publications 2021-07-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf