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contributor authorNoh, Yign
contributor authorGoh, Gahyun
contributor authorRaasch, Siegfried
date accessioned2017-06-09T16:36:40Z
date available2017-06-09T16:36:40Z
date copyright2010/09/01
date issued2010
identifier issn0022-3670
identifier otherams-70900.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212731
description abstractAnalysis of large-eddy simulation data of the ocean mixed layer under convection reveals that the contribution from wind stress decreases with time as a result of inertial oscillation in the extratropical ocean and that it leads to a rapid increase of the bulk and gradient Richardson number at the mixed layer depth. The criteria for the mixed layer deepening in the widely used mixed layer models, such as the Niiler?Kraus (NK) model, the Price?Weller?Pinkel (PWP) model, and the K-profile parameterization (KPP) model, are examined in view of these results, and its implication on the model predictability is discussed.
publisherAmerican Meteorological Society
titleExamination of the Mixed Layer Deepening Process during Convection Using LES
typeJournal Paper
journal volume40
journal issue9
journal titleJournal of Physical Oceanography
identifier doi10.1175/2010JPO4277.1
journal fristpage2189
journal lastpage2195
treeJournal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 009
contenttypeFulltext


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