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

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 terrain,...

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Bibliographic Details
Published in:The Cryosphere
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 in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-15-3059-2021
https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf
https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db