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contributor authorMorel, Y. G.
date accessioned2017-06-09T14:51:54Z
date available2017-06-09T14:51:54Z
date copyright1995/12/01
date issued1995
identifier issn0022-3670
identifier otherams-28459.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165577
description abstractIn this study, the effect of an upper-layer current on the propagation of intermediate vortices, such as Mediterranean Water eddies, is investigated. The author discusses the advection mechanism proposed by Hogg and Stommel and shows how the vertical shear of the mean current can also modify the dynamics of an eddy, acting as a gradient source of background potential vorticity.
publisherAmerican Meteorological Society
titleThe Influence of an Upper Thermocline Current on Intrathermocline Eddies
typeJournal Paper
journal volume25
journal issue12
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1995)025<3247:TIOAUT>2.0.CO;2
journal fristpage3247
journal lastpage3252
treeJournal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 012
contenttypeFulltext


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