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contributor authorBretherton, Christopher S.
date accessioned2017-06-09T14:27:27Z
date available2017-06-09T14:27:27Z
date copyright1987/07/01
date issued1987
identifier issn0022-4928
identifier otherams-19571.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155702
description abstractIntegral methods are used to show that in a simple model of nonprecipitating, moist convection, no small-amplitude propagating or oscillatory, two- or three-dimensional convective instabilities can grow from a quiescent basic state. This result holds for an inviscid layer with vertically varying stratification (of either finite or infinite depth) and for a uniformly stratified viscous layer of finite depth. The implications for the theory of wave-CISK are discussed.
publisherAmerican Meteorological Society
titleLinear Propagating Nonprecipitating Moist Convection
typeJournal Paper
journal volume44
journal issue14
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1987)044<1869:LPNMC>2.0.CO;2
journal fristpage1869
journal lastpage1874
treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 014
contenttypeFulltext


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