Suppression of Eddy Diffusivity across Jets in the Southern Ocean
Geostrophic eddies control the meridional mixing of heat, carbon, and other climatically important tracers in the Southern Ocean. The rate of eddy mixing is typically quantified through an eddy diffusivity. There is an ongoing debate as to whether eddy mixing in enhanced in the core of the Antarctic...
Prif Awduron: | Ferrari, Raffaele, Nikurashin, Maxim Anatolevich |
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Awduron Eraill: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
Fformat: | Erthygl |
Iaith: | en_US |
Cyhoeddwyd: |
American Meteorological Society
2011
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Mynediad Ar-lein: | http://hdl.handle.net/1721.1/62572 https://orcid.org/0000-0002-3736-1956 |
Eitemau Tebyg
Estimating Suppression of Eddy Mixing by Mean Flows
gan: Klocker, Andreas, et al.
Cyhoeddwyd: (2013)
gan: Klocker, Andreas, et al.
Cyhoeddwyd: (2013)
Eitemau Tebyg
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Cyhoeddwyd: (2014) -
The Impact of Finite-Amplitude Bottom Topography on Internal Wave Generation in the Southern Ocean
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Cyhoeddwyd: (2015) -
Global energy conversion rate from geostrophic flows into internal lee waves in the deep ocean
gan: Nikurashin, Maxim Anatolevich, et al.
Cyhoeddwyd: (2012) -
Eddy stirring in the Southern Ocean
gan: Ferrari, Raffaele, et al.
Cyhoeddwyd: (2012) -
Influence of Enhanced Abyssal Diapycnal Mixing on Stratification and the Ocean Overturning Circulation
gan: Nikurashin, Maxim Anatolevich, et al.
Cyhoeddwyd: (2016)