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    Interactions between Long and Synoptic-Scale Waves. Part I: Instability of a Nonzonal Flow

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 004::page 441
    Author:
    Ebisuzaiu, Wesley
    DOI: 10.1175/1520-0469(1989)046<0441:IBLASS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The interactions between long and synoptic-scale waves are studied as a two time-scale process. In the frame of reference of a long wave, a long wave varies slowly compared with the period of synoptic-scale waves. The long wave can spatially modulate the synoptic-scale waves whose fluxes will then show variations with the same wavelength as the long wave. These eddy fluxes can then alter the initial long wave on the slower time scale, making the interactions nonlinear. The assumption is made that the synoptic-scale waves have the structure ofthe most unstable normal modes; so in Part I, the instabilities of a wavy flow in a two-level j3-plane channel are studied. The derived analyticalsolution is simple, and appears more amenable to physical interpretation than previously derived analytical and numerical solutions The solution can be understood in terms of eddies and their local growth rate. In Part11, we will examine the effect of these synoptic-eddy fluxes on a long wave.
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      Interactions between Long and Synoptic-Scale Waves. Part I: Instability of a Nonzonal Flow

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4156193
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    contributor authorEbisuzaiu, Wesley
    date accessioned2017-06-09T14:28:46Z
    date available2017-06-09T14:28:46Z
    date copyright1989/02/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-20011.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156193
    description abstractThe interactions between long and synoptic-scale waves are studied as a two time-scale process. In the frame of reference of a long wave, a long wave varies slowly compared with the period of synoptic-scale waves. The long wave can spatially modulate the synoptic-scale waves whose fluxes will then show variations with the same wavelength as the long wave. These eddy fluxes can then alter the initial long wave on the slower time scale, making the interactions nonlinear. The assumption is made that the synoptic-scale waves have the structure ofthe most unstable normal modes; so in Part I, the instabilities of a wavy flow in a two-level j3-plane channel are studied. The derived analyticalsolution is simple, and appears more amenable to physical interpretation than previously derived analytical and numerical solutions The solution can be understood in terms of eddies and their local growth rate. In Part11, we will examine the effect of these synoptic-eddy fluxes on a long wave.
    publisherAmerican Meteorological Society
    titleInteractions between Long and Synoptic-Scale Waves. Part I: Instability of a Nonzonal Flow
    typeJournal Paper
    journal volume46
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1989)046<0441:IBLASS>2.0.CO;2
    journal fristpage441
    journal lastpage449
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 004
    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
    yabeshDSpacePersian