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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Bibliographic Details
Main Author: T. Heinze
Format: Article
Language:English
Published: Copernicus Publications 2025-04-01
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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