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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Библиографические подробности
Главные авторы: Lionel Renault, S. Masson, T. Arsouze, Gurvan Madec, James C. McWilliams
Формат: Artigo
Язык:Inglês
Опубликовано: American Geophysical Union (AGU) 2020-02-01
Серии:Journal of Advances in Modeling Earth Systems
Предметы:
Air‐Sea interaction
Current Feedback
Parameterization
Forced Ocean Model
Reanalysis
Scatterometers
Online-ссылка:https://doi.org/10.1029/2019MS001715
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