Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory
Observations and inverse models suggest that small-scale turbulent mixing is enhanced in the Southern Ocean in regions above rough topography. The enhancement extends O(1) km above the topography, suggesting that mixing is supported by the breaking of gravity waves radiated from the ocean bottom. In...
| Asıl Yazarlar: | , |
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| Materyal Türü: | Makale |
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American Meteorological Society
2018
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| Online Erişim: | http://hdl.handle.net/1721.1/118188 https://orcid.org/0000-0002-3736-1956 |