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...

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Detalles Bibliográficos
Autores principales: Shackelford, Kyle, DeMott, Charlotte A., van Leeuwen, Peter Jan, Thompson, Elizabeth, Hagos, Samson
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
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

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9286434/
https://www.ncbi.nlm.nih.gov/pubmed/35865796
http://dx.doi.org/10.1029/2021JC018025

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