Dynamics of an Abyssal Circulation Driven by Bottom-Intensified Mixing on Slopes
The large-scale circulation of the abyssal ocean is enabled by small-scale diapycnal mixing, which observations suggest is strongly enhanced toward the ocean bottom, where the breaking of internal tides and lee waves is most vigorous. As discussed recently, bottom-intensified mixing induces a patter...
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| Natura: | Articolo |
| Lingua: | English |
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American Meteorological Society
2020
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| Accesso online: | https://hdl.handle.net/1721.1/125088 |