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Local atmospheric response to warm mesoscale ocean eddies in the Kuroshio–Oyashio Confluence region

In the extratropical regions, surface winds enhance upward heat release from the ocean to atmosphere, resulting in cold surface ocean: surface ocean temperature is negatively correlated with upward heat flux. However, in the western boundary currents and eddy-rich regions, the warmer surface waters...

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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Sugimoto, Shusaku, Aono, Kenji, Fukui, Shin
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2017
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5605681/
https://ncbi.nlm.nih.gov/pubmed/28928408
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-12206-9
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