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...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-07-01
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Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf |