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    Practical Application of Two-Turning-Point Theory to Mountain-Wave Transmission through a Wind Jet

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 002::page 481
    Author:
    Broutman, Dave
    ,
    Eckermann, Stephen D.
    ,
    Rottman, James W.
    DOI: 10.1175/2008JAS2786.1
    Publisher: American Meteorological Society
    Abstract: A Fourier method is used to model mountain waves that have nearby turning points in a wind jet. In Fourier space, the propagation equations are solved by ray theory. To correct for the ray singularity at a turning point without time-consuming special-function evaluations, the ray solution is linearly interpolated across the breakdown region. The Fourier solutions for the spatial wavefield are compared with mesoscale model simulations in two cases: two-dimensional flow over idealized topography with uniform stratification and a sech-squared wind profile and three-dimensional flow over the island of Jan Mayen with stratification and wind profiles taken from radiosonde measurements. The latter case reveals the partial transmission of trapped mountain waves into the stratosphere.
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      Practical Application of Two-Turning-Point Theory to Mountain-Wave Transmission through a Wind Jet

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208257
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    contributor authorBroutman, Dave
    contributor authorEckermann, Stephen D.
    contributor authorRottman, James W.
    date accessioned2017-06-09T16:23:00Z
    date available2017-06-09T16:23:00Z
    date copyright2009/02/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-66873.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208257
    description abstractA Fourier method is used to model mountain waves that have nearby turning points in a wind jet. In Fourier space, the propagation equations are solved by ray theory. To correct for the ray singularity at a turning point without time-consuming special-function evaluations, the ray solution is linearly interpolated across the breakdown region. The Fourier solutions for the spatial wavefield are compared with mesoscale model simulations in two cases: two-dimensional flow over idealized topography with uniform stratification and a sech-squared wind profile and three-dimensional flow over the island of Jan Mayen with stratification and wind profiles taken from radiosonde measurements. The latter case reveals the partial transmission of trapped mountain waves into the stratosphere.
    publisherAmerican Meteorological Society
    titlePractical Application of Two-Turning-Point Theory to Mountain-Wave Transmission through a Wind Jet
    typeJournal Paper
    journal volume66
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2786.1
    journal fristpage481
    journal lastpage494
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 002
    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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