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    Direct Calculation of Low-Frequency Coastally Trapped Waves and Their Scattering

    Source: Journal of Atmospheric and Oceanic Technology:;1993:;volume( 010 ):;issue: 003::page 368
    Author:
    Schmidt, G. A.
    ,
    Johnson, E. R.
    DOI: 10.1175/1520-0426(1993)010<0368:DCOLFC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new, direct numerical method is proposed for finding the phase speeds and pressure fields of low-frequency nondispersive coastally trapped waves in a continuously stratified flow. The usual two-dimensional problem is reduced to a one-dimensional integral equation across the shelf. The structure of the problem depends on the strength of the stratification measured by the parameter B = NoD/fL for typical buoyancy frequency No, depth D, Coriolis parameter f, and shelf width L. Asymptotic approximations are given for both strong (B?1) and weak (B ? 1) stratification, and attempts are made to provide analytical expressions for the phase speeds over the whole range of B using Padé approximations. These compare well with the numerical results. Examples are given using a number of different topographies and the conditions for which mode kissing between baroclinic and barotropic wave modes occur are discussed. The method is particularly suited to evaluating the scattering for waves moving from one topography to another.
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      Direct Calculation of Low-Frequency Coastally Trapped Waves and Their Scattering

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223956
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorSchmidt, G. A.
    contributor authorJohnson, E. R.
    date accessioned2017-06-09T17:12:04Z
    date available2017-06-09T17:12:04Z
    date copyright1993/06/01
    date issued1993
    identifier issn0739-0572
    identifier otherams-810.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223956
    description abstractA new, direct numerical method is proposed for finding the phase speeds and pressure fields of low-frequency nondispersive coastally trapped waves in a continuously stratified flow. The usual two-dimensional problem is reduced to a one-dimensional integral equation across the shelf. The structure of the problem depends on the strength of the stratification measured by the parameter B = NoD/fL for typical buoyancy frequency No, depth D, Coriolis parameter f, and shelf width L. Asymptotic approximations are given for both strong (B?1) and weak (B ? 1) stratification, and attempts are made to provide analytical expressions for the phase speeds over the whole range of B using Padé approximations. These compare well with the numerical results. Examples are given using a number of different topographies and the conditions for which mode kissing between baroclinic and barotropic wave modes occur are discussed. The method is particularly suited to evaluating the scattering for waves moving from one topography to another.
    publisherAmerican Meteorological Society
    titleDirect Calculation of Low-Frequency Coastally Trapped Waves and Their Scattering
    typeJournal Paper
    journal volume10
    journal issue3
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1993)010<0368:DCOLFC>2.0.CO;2
    journal fristpage368
    journal lastpage380
    treeJournal of Atmospheric and Oceanic Technology:;1993:;volume( 010 ):;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