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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Format: | Text |
Language: | English |
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2021
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Online Access: | https://doi.org/10.5194/tc-2021-60 https://tc.copernicus.org/preprints/tc-2021-60/ |