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Topographic generation of submesoscale centrifugal instability and energy dissipation
Most of the ocean kinetic energy is contained in the large scale currents and the vigorous geostrophic eddy field, at horizontal scales of order 100 km. To achieve equilibrium the geostrophic currents must viscously dissipate their kinetic energy at much smaller scale. However, geostrophic turbulenc...
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| 出版年: | Nat Commun |
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| 主要な著者: | , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group
2016
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5056419/ https://ncbi.nlm.nih.gov/pubmed/27681822 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms12811 |
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