Capillary suction across the soil–snow interface as a mechanism for the formation of wet basal layers under gliding snowpacks
Capillary suction across the soil–snow interface is a possible mechanism for the formation of wet basal snow layers, which are necessary for snow gliding and glide-snow avalanches. However, little is known about the conditions under which this process occurs. We investigated capillary suction across...
| Published in: | Journal of Glaciology |
|---|---|
| Main Authors: | , , , , , , |
| Format: | Article |
| Language: | English |
| Published: |
Cambridge University Press
2025-01-01
|
| Subjects: | |
| Online Access: | https://www.cambridge.org/core/product/identifier/S0022143025000024/type/journal_article |
