A conjecture on the role of bottom-enhanced diapycnal mixing in the parameterization of geostrophic eddies
Marshall, David P. and Naveira Garabato, Alberto C. (2008) A conjecture on the role of bottom-enhanced diapycnal mixing in the parameterization of geostrophic eddies. Journal of Physical Oceanography, 38, (7), 1607-1613. (doi:10.1175/2007JPO3619.1).
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The parameterization of geostrophic eddies represents a large sink of energy in most ocean models, yet the ultimate fate of this eddy energy in the ocean remains unclear. The authors conjecture that a significant fraction of the eddy energy may be transferred to internal lee waves and oscillations over rough bottom topography, leading to bottom-enhanced diapycnal mixing. A range of circumstantial evidence in support of this conjecture is presented and discussed. The authors further propose a modification to the Gent and McWilliams eddy parameterization to account for the bottom-enhanced diapycnal mixing.
|Subjects:||Q Science > Q Science (General)
G Geography. Anthropology. Recreation > GC Oceanography
Q Science > QC Physics
|Divisions:||University Structure - Pre August 2011 > School of Ocean & Earth Science (SOC/SOES)
|Date Deposited:||24 May 2006|
|Last Modified:||01 Jun 2011 16:36|
|Contributors:||Marshall, David P. (Author)
Naveira Garabato, Alberto C. (Author)
|Contact Email Address:||email@example.com|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
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