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contributor authorFarrell, Brian F.
contributor authorIoannou, Petros J.
date accessioned2017-06-09T14:31:58Z
date available2017-06-09T14:31:58Z
date copyright1993/12/01
date issued1993
identifier issn0022-4928
identifier otherams-21090.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157391
description abstractThe maintenance of variance and attendant heat flux in linear, forced, dissipative baroclinic shear flows subject to stochastic excitation is examined. The baroclinic problem is intrinsically nonnormal and its stochastic dynamics is found to differ significantly from the more familiar stochastic dynamics of normal systems. When the shear is sufficiently great in comparison to dissipative effects, stochastic excitation supports highly enhanced variance levels in these nonnormal systems compared to variance levels supported by the same forcing and dissipation in related normal systems. The eddy variance and associated heat flux are found to arise in response to transient amplification of a subset of forcing functions that obtain energy from the mean flow and project this energy on a distinct subset of response functions (E0Fs) that are in turn distinct from the set of normal modes of the system. A method for obtaining the dominant forcing and response functions as well as the distribution of heat flux for a given flow is described.
publisherAmerican Meteorological Society
titleStochastic Dynamics of Baroclinic Waves
typeJournal Paper
journal volume50
journal issue24
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1993)050<4044:SDOBW>2.0.CO;2
journal fristpage4044
journal lastpage4057
treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 024
contenttypeFulltext


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