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    Exponentially Small Inertia–Gravity Waves and the Breakdown of Quasigeostrophic Balance

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 002::page 211
    Author:
    Vanneste, J.
    ,
    Yavneh, I.
    DOI: 10.1175/1520-0469(2004)061<0211:ESIWAT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The spontaneous generation of inertia?gravity waves by balanced motion is investigated in the limit of small Rossby number ? ? 1. Particular (sheared disturbance) solutions of the three-dimensional Boussinesq equations are considered. For these solutions, there is a strict separation between balanced motion and inertia?gravity waves for large times. This makes it possible to estimate the amplitude of the inertia?gravity waves that are generated spontaneously from perfectly balanced initial conditions. It is shown analytically using exponential asymptotics, and confirmed numerically, that this amplitude is proportional to ??1/2 exp(?α/?), with a constant α > 0 and a proportionality constant that are given in closed form. This result demonstrates the inevitability of inertia?gravity wave generation and hence the nonexistence of an invariant slow manifold; it also exemplifies the remarkable, exponential, smallness of the wave generation for ? ? 1. The importance of the singularity structure of the balanced motion for complex values of time is emphasized, and some general implications of the results are discussed.
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      Exponentially Small Inertia–Gravity Waves and the Breakdown of Quasigeostrophic Balance

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159970
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    • Journal of the Atmospheric Sciences

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    contributor authorVanneste, J.
    contributor authorYavneh, I.
    date accessioned2017-06-09T14:38:32Z
    date available2017-06-09T14:38:32Z
    date copyright2004/01/01
    date issued2004
    identifier issn0022-4928
    identifier otherams-23411.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159970
    description abstractThe spontaneous generation of inertia?gravity waves by balanced motion is investigated in the limit of small Rossby number ? ? 1. Particular (sheared disturbance) solutions of the three-dimensional Boussinesq equations are considered. For these solutions, there is a strict separation between balanced motion and inertia?gravity waves for large times. This makes it possible to estimate the amplitude of the inertia?gravity waves that are generated spontaneously from perfectly balanced initial conditions. It is shown analytically using exponential asymptotics, and confirmed numerically, that this amplitude is proportional to ??1/2 exp(?α/?), with a constant α > 0 and a proportionality constant that are given in closed form. This result demonstrates the inevitability of inertia?gravity wave generation and hence the nonexistence of an invariant slow manifold; it also exemplifies the remarkable, exponential, smallness of the wave generation for ? ? 1. The importance of the singularity structure of the balanced motion for complex values of time is emphasized, and some general implications of the results are discussed.
    publisherAmerican Meteorological Society
    titleExponentially Small Inertia–Gravity Waves and the Breakdown of Quasigeostrophic Balance
    typeJournal Paper
    journal volume61
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2004)061<0211:ESIWAT>2.0.CO;2
    journal fristpage211
    journal lastpage223
    treeJournal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 002
    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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