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    Internal Gravity Waves in an Atmosphere with Wind Shear: Validity of the WKB Approximation at Critical Layers in the Presence of Buoyancy Forces

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 002::page 313
    Author:
    Whitten, R. C.
    ,
    Riegel, C. A.
    DOI: 10.1175/1520-0469(1973)030<0313:IGWIAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The application of the WKB method to internal gravity waves in a compressible fluid with wind shear is studied from the standpoint of dispersion and of the validity of the method. It is shown that at resonance (the level where the phase speed is Doppler-shifted to zero) the validity is dependent only on the local Richardson number; we accept as the criterion that Ri?1. The wave attenuation obtained by means of the WKB method is very close to that obtained from the ?exact? solution.
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      Internal Gravity Waves in an Atmosphere with Wind Shear: Validity of the WKB Approximation at Critical Layers in the Presence of Buoyancy Forces

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4152103
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    contributor authorWhitten, R. C.
    contributor authorRiegel, C. A.
    date accessioned2017-06-09T14:16:50Z
    date available2017-06-09T14:16:50Z
    date copyright1973/03/01
    date issued1973
    identifier issn0022-4928
    identifier otherams-16331.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152103
    description abstractThe application of the WKB method to internal gravity waves in a compressible fluid with wind shear is studied from the standpoint of dispersion and of the validity of the method. It is shown that at resonance (the level where the phase speed is Doppler-shifted to zero) the validity is dependent only on the local Richardson number; we accept as the criterion that Ri?1. The wave attenuation obtained by means of the WKB method is very close to that obtained from the ?exact? solution.
    publisherAmerican Meteorological Society
    titleInternal Gravity Waves in an Atmosphere with Wind Shear: Validity of the WKB Approximation at Critical Layers in the Presence of Buoyancy Forces
    typeJournal Paper
    journal volume30
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1973)030<0313:IGWIAA>2.0.CO;2
    journal fristpage313
    journal lastpage316
    treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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