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contributor authorSmith, Ronald B.
contributor authorSun, Jielun
date accessioned2017-06-09T14:27:41Z
date available2017-06-09T14:27:41Z
date copyright1987/10/01
date issued1987
identifier issn0022-4928
identifier otherams-19648.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155787
description abstractNonlinear steady-state solutions for stratified two-layer flow over a ridge are found. In parameter space, these solutions lie between the interfacial case of Long and the constant stratification case of Smith. The solutions predict the depth of the layer which will descend and accelerate. Qualitative agreement with Bora and Boulder observations is found.
publisherAmerican Meteorological Society
titleGeneralized Hydraulic Solutions Pertaining to Severe Downslope Winds
typeJournal Paper
journal volume44
journal issue20
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1987)044<2934:GHSPTS>2.0.CO;2
journal fristpage2934
journal lastpage2939
treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 020
contenttypeFulltext


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