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

Abstract 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 s...

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Detalhes bibliográficos

Principais autores:	Frans‐Jan W. Parmentier, Lennart Nilsen, Hans Tømmervik, Ove H. Meisel, Lisa Bröder, Jorien E. Vonk, Sebastian Westermann, Philipp R. Semenchuk, Elisabeth J. Cooper
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2024-06-01
coleção:	Geophysical Research Letters
Assuntos:	permafrost thermokarst snow cover runoff soil carbon dissolved organic carbon
Acesso em linha:	https://doi.org/10.1029/2023GL108020
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