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contributor authorFritts, David C.
date accessioned2017-06-09T14:21:40Z
date available2017-06-09T14:21:40Z
date copyright1980/07/01
date issued1980
identifier issn0022-4928
identifier otherams-17964.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153916
description abstractPrevious studies have revealed a number of unstable modes in addition to the Kelvin-Helmholtz instability associated with a velocity shear in the presence of a rigid lower boundary. These additional modes occupy regions in the (α,Ri0) plane which are largely distinct from that occupied by the Kelvin-Helmholtz mode. In this note, we demonstrate that the location of the various unstable modes can be explained in part in terms of the modal structure above and below the velocity shear and the necessary condition for dynamical instability, Ric < 1/4, obtained by Miles (1961). An extension of the stability analysis of Lalas and Einaudi (1976) to a larger shear height reveals that all unstable modes belong to one of two mode families. Finally, we discuss the implication of these results for additional modes or families of modes and the possible roles of various modes in atmospheric dynamics.
publisherAmerican Meteorological Society
titleSimple Stability Limits for Vertically Propagating Unstable Modes in a tanh(z) Velocity Profile with a Rigid Lower Boundary
typeJournal Paper
journal volume37
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1980)037<1642:SSLFVP>2.0.CO;2
journal fristpage1642
journal lastpage1648
treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 007
contenttypeFulltext


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