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Rain‐Induced Stratification of the Equatorial Indian Ocean and Its Potential Feedback to the Atmosphere
Surface freshening through precipitation can act to stably stratify the upper ocean, forming a rain layer (RL). RLs inhibit subsurface vertical mixing, isolating deeper ocean layers from the atmosphere. This process has been studied using observations and idealized simulations. The present ocean mod...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286434/ https://www.ncbi.nlm.nih.gov/pubmed/35865796 http://dx.doi.org/10.1029/2021JC018025 |