Effects of subgrid-scale ice topography on the ice shelf basal melting simulated in NEMO-4.2.0
<p>At the interface between the ocean and the ice shelf base, in the framework of the shear-controlled melt parameterisation, the ice melts due to combined actions of temperature, salinity and friction velocity. In the NEMO ocean model, the friction velocity is usually computed based on a constant d...
Guardat en:
| Autors principals: | , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Copernicus Publications
2026-04-01
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| Col·lecció: | The Cryosphere |
| Accés en línia: | https://tc.copernicus.org/articles/20/1997/2026/tc-20-1997-2026.pdf |
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