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    On the Forcing of Inertia–Gravity Waves by Synoptic-Scale Flows

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 005::page 1737
    Author:
    Plougonven, Riwal
    ,
    Zhang, Fuqing
    DOI: 10.1175/JAS3901.1
    Publisher: American Meteorological Society
    Abstract: Studies 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.
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      On the Forcing of Inertia–Gravity Waves by Synoptic-Scale Flows

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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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