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contributor authorMarshall, David P.
contributor authorWilliams, Richard G.
contributor authorLee, Mei-Man
date accessioned2017-06-09T14:53:33Z
date available2017-06-09T14:53:33Z
date copyright1999/07/01
date issued1999
identifier issn0022-3670
identifier otherams-29065.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166251
description abstractThe dynamical control of the eddy-induced transport is investigated in a series of idealized eddy-resolving experiments. When there is an active eddy field, the eddy-induced transport is found to correlate with isopycnic gradients of potential vorticity, rather than gradients of layer thickness. For any unforced layers, the eddy transfer leads to a homogenization of potential vorticity and a vanishing of the eddy-induced transport in the final steady state.
publisherAmerican Meteorological Society
titleThe Relation between Eddy-Induced Transport and Isopycnic Gradients of Potential Vorticity
typeJournal Paper
journal volume29
journal issue7
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1999)029<1571:TRBEIT>2.0.CO;2
journal fristpage1571
journal lastpage1578
treeJournal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 007
contenttypeFulltext


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