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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5605681/ https://www.ncbi.nlm.nih.gov/pubmed/28928408 http://dx.doi.org/10.1038/s41598-017-12206-9 |