Journal
JOURNAL OF MARINE RESEARCH
Volume 68, Issue 3-4, Pages 479-502Publisher
SEARS FOUNDATION MARINE RESEARCH
DOI: 10.1357/002224010794657227
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Funding
- National Science Foundation [MCA06N007, OCE 0927583]
- Directorate For Geosciences
- Division Of Ocean Sciences [0927583] Funding Source: National Science Foundation
- Division Of Ocean Sciences
- Directorate For Geosciences [0822075] Funding Source: National Science Foundation
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The relation between topography, and the 3D structure of patchy eddy-induced mixing in the Southern Ocean is analyzed descriptively by applying diagnostic methods to output from the Southern Ocean State Estimate. A localized cumulative probability density function method is developed to verify the use of Nakamura's (2001) mixing efficiency in the ocean. Both methods reveal enhanced eddy mixing at mid-depths. The spatial pattern of the mid-depth enhancement of eddy mixing is primarily linked to the merging of multiple jets embedded in the Antarctic Circumpolar Current over topography. We suggest that enhanced eddy mixing over topography is due to locally enhanced baroclinicity and instability within the wake itself, partly due to the convergence of eddies in merging branches of the ACC. Interaction of barotropic and baroclinic eddies may be important to setting the strength and vertical structure of eddy mixing associated with topography.
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