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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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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2017
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| Témata: | |
| On-line přístup: | 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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