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    The Scattering of Rossby Waves by a Semi-Infinite Barrier

    Source: Journal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 001::page 108
    Author:
    Mysak, L. A.
    ,
    LeBlond, P. H.
    DOI: 10.1175/1520-0485(1972)002<0108:TSORWB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We discuss the scattering of divergent Rossby waves by a semi-infinite vertical barrier of arbitrary orientation on a ? plane. The Wiener-Hopf method is used to obtain an integral representation of the scattered wave field which, in turn, gives explicit expressions for the scattered velocity components along the axis of the barrier and the pressure difference across the barrier. Far from the corner of the barrier the solution, in part, consists of a scattered wave whose amplitude falls off as 1/r½ but whose phase travels radially inward and at the same time advects westward. Also, the barrier gives rise to the familiar reflected wave and shadow zone regions. However, because of the anisotropic nature of Rossby waves, these regions are determined by the direction of incident energy propagation, which is always different from the direction of the incident phase velocity.
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      The Scattering of Rossby Waves by a Semi-Infinite Barrier

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162061
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    contributor authorMysak, L. A.
    contributor authorLeBlond, P. H.
    date accessioned2017-06-09T14:43:33Z
    date available2017-06-09T14:43:33Z
    date copyright1972/01/01
    date issued1972
    identifier issn0022-3670
    identifier otherams-25294.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162061
    description abstractWe discuss the scattering of divergent Rossby waves by a semi-infinite vertical barrier of arbitrary orientation on a ? plane. The Wiener-Hopf method is used to obtain an integral representation of the scattered wave field which, in turn, gives explicit expressions for the scattered velocity components along the axis of the barrier and the pressure difference across the barrier. Far from the corner of the barrier the solution, in part, consists of a scattered wave whose amplitude falls off as 1/r½ but whose phase travels radially inward and at the same time advects westward. Also, the barrier gives rise to the familiar reflected wave and shadow zone regions. However, because of the anisotropic nature of Rossby waves, these regions are determined by the direction of incident energy propagation, which is always different from the direction of the incident phase velocity.
    publisherAmerican Meteorological Society
    titleThe Scattering of Rossby Waves by a Semi-Infinite Barrier
    typeJournal Paper
    journal volume2
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1972)002<0108:TSORWB>2.0.CO;2
    journal fristpage108
    journal lastpage114
    treeJournal of Physical Oceanography:;1972:;Volume( 002 ):;issue: 001
    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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