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: Hamm, Alexandra, Frampton, Andrew
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-4853-2021
https://noa.gwlb.de/receive/cop_mods_00058437
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00058079/tc-15-4853-2021.pdf
https://tc.copernicus.org/articles/15/4853/2021/tc-15-4853-2021.pdf