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Wave–turbulence interaction-induced vertical mixing and its effects in ocean and climate models
Heated from above, the oceans are stably stratified. Therefore, the performance of general ocean circulation models and climate studies through coupled atmosphere–ocean models depends critically on vertical mixing of energy and momentum in the water column. Many of the traditional general circulatio...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
The Royal Society Publishing
2016
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4792408/ https://www.ncbi.nlm.nih.gov/pubmed/26953182 http://dx.doi.org/10.1098/rsta.2015.0201 |