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contributor authorPlougonven, Riwal
contributor authorZhang, Fuqing
date accessioned2017-06-09T16:53:37Z
date available2017-06-09T16:53:37Z
date copyright2007/05/01
date issued2007
identifier issn0022-4928
identifier otherams-76084.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218492
description abstractStudies on the spontaneous emission of gravity waves from jets, both observational and numerical, have emphasized that excitation of gravity waves occurred preferentially near regions of imbalance. Yet a quantitative relation between the several large-scale diagnostics of imbalance and the excited waves is still lacking. The purpose of the present note is to investigate one possible way to relate quantitatively the gravity waves to diagnostics of the large-scale flow that is exciting them. Scaling arguments are used to determine how the large-scale flow may provide a forcing on the right-hand side of a wave equation describing the linear dynamics of the excited waves. The residual of the nonlinear balance equation plays an important role in this forcing.
publisherAmerican Meteorological Society
titleOn the Forcing of Inertia–Gravity Waves by Synoptic-Scale Flows
typeJournal Paper
journal volume64
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS3901.1
journal fristpage1737
journal lastpage1742
treeJournal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 005
contenttypeFulltext


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