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...
| Published in: | The Cryosphere |
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| Main Authors: | , |
| Format: | Text |
| Language: | English |
| Published: |
2021
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/tc-15-4853-2021 https://tc.copernicus.org/articles/15/4853/2021/ |