A local thermal non-equilibrium model for rain-on-snow events
<p>Liquid-water movement through a snowpack, e.g., during rain-on-snow events or meltwater infiltration, is an essential process to understand runoff generation, flash floods, and snow avalanches. From a physical point of view, water infiltration into snow is a strongly coupled thermo-hydrauli...
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| Main Author: | |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-04-01
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| Series: | Hydrology and Earth System Sciences |
| Online Access: | https://hess.copernicus.org/articles/29/2059/2025/hess-29-2059-2025.pdf |
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