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...

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Detalles Bibliográficos
Autores principales: Hummels, Rebecca, Dengler, Marcus, Rath, Willi, Foltz, Gregory R., Schütte, Florian, Fischer, Tim, Brandt, Peter
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
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

Internet

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

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