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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...
में बचाया:
| में प्रकाशित: | Philos Trans A Math Phys Eng Sci |
|---|---|
| मुख्य लेखकों: | , , , , |
| स्वरूप: | Artigo |
| भाषा: | Inglês |
| प्रकाशित: |
The Royal Society Publishing
2016
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| विषय: | |
| ऑनलाइन पहुंच: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4792408/ https://ncbi.nlm.nih.gov/pubmed/26953182 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2015.0201 |
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