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A simulation of a large-scale drifting snowstorm in the turbulent boundary layer
<p>Drifting snowstorms are an important aeolian process that reshape alpine glaciers and polar ice shelves, and they may also affect the climate system and hydrological cycle since flying snow particles exchange considerable mass and energy with air flow. Prior studies have rarely considered f...
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Main Authors: | , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
Copernicus Publications
2018-12-01
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Colecção: | The Cryosphere |
Acesso em linha: | https://www.the-cryosphere.net/12/3841/2018/tc-12-3841-2018.pdf |
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