Rapid Ice‐Wedge Collapse and Permafrost Carbon Loss Triggered by Increased Snow Depth and Surface Runoff

Thicker snow cover in permafrost areas causes deeper active layers and thaw subsidence, which alter local hydrology and may amplify the loss of soil carbon. However, the potential for changes in snow cover and surface runoff to mobilize permafrost carbon remains poorly quantified. In this study, we...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Parmentier, Frans-Jan W., Nilsen, Lennart, Tømmervik, Hans, Meisel, Ove H., Bröder, Lisa, Vonk, Jorien E., Westermann, Sebastian, Semenchuk, Phillip R., Cooper, Elisabeth J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Ice
Online Access:https://hdl.handle.net/10037/33773
https://doi.org/10.1029/2023GL108020