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contributor authorCanuto, V. M.
contributor authorCheng, Y.
contributor authorHoward, A. M.
contributor authorEsau, I. N.
date accessioned2017-06-09T16:18:51Z
date available2017-06-09T16:18:51Z
date copyright2008/07/01
date issued2008
identifier issn0022-4928
identifier otherams-65571.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206810
description abstractA large set of laboratory, direct numerical simulation (DNS), and large eddy simulation (LES) data indicates that in stably stratified flows turbulent mixing exists up to Ri ? O(100), meaning that there is practically no Ri(cr). On the other hand, traditional local second-order closure (SOC) models entail a critical Ri(cr) ? O(1) above which turbulence ceases to exist and are therefore unable to explain the above data. The authors suggest how to modify the recent SOC model of Cheng et al. to reproduce the above data for arbitrary Ri.
publisherAmerican Meteorological Society
titleStably Stratified Flows: A Model with No Ri(cr)
typeJournal Paper
journal volume65
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2007JAS2470.1
journal fristpage2437
journal lastpage2447
treeJournal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 007
contenttypeFulltext


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