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    Scattering of Sound by Internal Wave Currents: The Relation to Vertical Momentum Flux

    Source: Journal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 004::page 442
    Author:
    Munk, W.
    ,
    Worcester, P.
    ,
    Zachariasen, F.
    DOI: 10.1175/1520-0485(1981)011<0442:SOSBIW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Internal waves scatter sound by two related perturbations: 1) those associated with vertical particle displacements ?(x, y, z, t) in the presence of a vertical gradient of (potential) sound speed (δc = ??zcp); and 2) those associated with horizontal particle velocities u(x, y, z, t). The combined fractional perturbation in propagation velocity is δc/c + u/c. The second term, generally neglected, introduces a nonreciprocity when source and receiver are interchanged. Nonreciprocity is expected to be relatively small except for transmission along a deep downward loop. The principal internal wave contribution to nonreciprocity is from inertial frequencies. The sum and difference of reciprocal travel times are a measure of ? and u, respectively, along the ray path,, the quadrature spectrum of reciprocal travel times is related by an integral equation to the spectrum of the momentum flux ??u?. Precise measurements of nonreciprocity could provide an estimate of the vertical momentum flux in an internal wave field.
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      Scattering of Sound by Internal Wave Currents: The Relation to Vertical Momentum Flux

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4163077
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    contributor authorMunk, W.
    contributor authorWorcester, P.
    contributor authorZachariasen, F.
    date accessioned2017-06-09T14:45:49Z
    date available2017-06-09T14:45:49Z
    date copyright1981/04/01
    date issued1981
    identifier issn0022-3670
    identifier otherams-26208.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163077
    description abstractInternal waves scatter sound by two related perturbations: 1) those associated with vertical particle displacements ?(x, y, z, t) in the presence of a vertical gradient of (potential) sound speed (δc = ??zcp); and 2) those associated with horizontal particle velocities u(x, y, z, t). The combined fractional perturbation in propagation velocity is δc/c + u/c. The second term, generally neglected, introduces a nonreciprocity when source and receiver are interchanged. Nonreciprocity is expected to be relatively small except for transmission along a deep downward loop. The principal internal wave contribution to nonreciprocity is from inertial frequencies. The sum and difference of reciprocal travel times are a measure of ? and u, respectively, along the ray path,, the quadrature spectrum of reciprocal travel times is related by an integral equation to the spectrum of the momentum flux ??u?. Precise measurements of nonreciprocity could provide an estimate of the vertical momentum flux in an internal wave field.
    publisherAmerican Meteorological Society
    titleScattering of Sound by Internal Wave Currents: The Relation to Vertical Momentum Flux
    typeJournal Paper
    journal volume11
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1981)011<0442:SOSBIW>2.0.CO;2
    journal fristpage442
    journal lastpage454
    treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;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
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