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Surface cooling caused by rare but intense near-inertial wave induced mixing in the tropical Atlantic
The direct response of the tropical mixed layer to near-inertial waves (NIWs) has only rarely been observed. Here, we present upper-ocean turbulence data that provide evidence for a strongly elevated vertical diffusive heat flux across the base of the mixed layer in the presence of a NIW, thereby co...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7395095/ https://www.ncbi.nlm.nih.gov/pubmed/32737290 http://dx.doi.org/10.1038/s41467-020-17601-x |