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    Rayleigh Wave–Internal Wave Coupling and Internal Wave Generation above a Model Jet Stream

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 003::page 1042
    Author:
    Sutherland, B. R.
    DOI: 10.1175/JAS3658.1
    Publisher: American Meteorological Society
    Abstract: Linear theory for modes in a nonuniformly stratified, semi-infinite shear flow demonstrates that Rayleigh waves (stable waves propagating in fluid with spatially varying shear) couple with evanescent internal waves. If the bulk Richardson number (the squared ratio of the buoyancy frequency and shear) lies between 1/4 and 1, the waves have infinite e-folding depth for waves with critical relative horizontal wavenumbers. Fully nonlinear numerical simulations examine the effect of Rayleigh wave?internal wave coupling when the shear layer is localized and is thus Kelvin?Helmholtz unstable. Diagnostics examining profiles of the wave-induced mean flow show that if the bulk Richardson number is of order unity, significant momentum is extracted from a shear layer as a consequence of transport by waves. The work is extended to the study of unstable jet flows and applications of this work for internal wave generation by dynamic instability of the upper flank of the jet stream are discussed.
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      Rayleigh Wave–Internal Wave Coupling and Internal Wave Generation above a Model Jet Stream

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4218225
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    contributor authorSutherland, B. R.
    date accessioned2017-06-09T16:52:48Z
    date available2017-06-09T16:52:48Z
    date copyright2006/03/01
    date issued2006
    identifier issn0022-4928
    identifier otherams-75844.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218225
    description abstractLinear theory for modes in a nonuniformly stratified, semi-infinite shear flow demonstrates that Rayleigh waves (stable waves propagating in fluid with spatially varying shear) couple with evanescent internal waves. If the bulk Richardson number (the squared ratio of the buoyancy frequency and shear) lies between 1/4 and 1, the waves have infinite e-folding depth for waves with critical relative horizontal wavenumbers. Fully nonlinear numerical simulations examine the effect of Rayleigh wave?internal wave coupling when the shear layer is localized and is thus Kelvin?Helmholtz unstable. Diagnostics examining profiles of the wave-induced mean flow show that if the bulk Richardson number is of order unity, significant momentum is extracted from a shear layer as a consequence of transport by waves. The work is extended to the study of unstable jet flows and applications of this work for internal wave generation by dynamic instability of the upper flank of the jet stream are discussed.
    publisherAmerican Meteorological Society
    titleRayleigh Wave–Internal Wave Coupling and Internal Wave Generation above a Model Jet Stream
    typeJournal Paper
    journal volume63
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS3658.1
    journal fristpage1042
    journal lastpage1055
    treeJournal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 003
    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