Impact of lateral groundwater flow on hydrothermal conditions of the active layer in a high-Arctic hillslope setting

Modeling the physical state of permafrost landscapes is a crucial addition to field observations in order to understand the feedback mechanisms between permafrost and the atmosphere within a warming climate. A common hypothesis in permafrost modeling is that vertical heat conduction is most relevant...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: A. Hamm, A. Frampton
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-4853-2021
https://doaj.org/article/a427a4fbbd58408b83fcd131b7e34454