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).
Full text not available from this repository.
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.
|Digital Object Identifier (DOI):||doi:10.1175/2007JPO3619.1|
|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:||31 Mar 2016 12:06|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
Actions (login required)