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 its feedback mechanisms within a warming climate. A common hypothesis in permafrost modeling is that vertical heat conduction is most relevant to derive subsurface temperatures. Wh...

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Bibliographic Details
Main Authors: Hamm, Alexandra, Frampton, Andrew
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-2021-60
https://tc.copernicus.org/preprints/tc-2021-60/