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Recipes for How to Force Oceanic Model Dynamics
Abstract The current feedback to the atmosphere (CFB) contributes to the oceanic circulation by damping eddies. In an ocean‐atmosphere coupled model, CFB can be correctly accounted for by using the wind relative to the oceanic current. However, its implementation in a forced oceanic model is less st...
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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Geophysical Union (AGU)
2020-02-01
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| Col·lecció: | Journal of Advances in Modeling Earth Systems |
| Matèries: | |
| Accés en línia: | https://doi.org/10.1029/2019MS001715 |
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