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    A Diagnostic Study of Waves on the Tropopause

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 012::page 3315
    Author:
    Tomikawa, Yoshihiro
    ,
    Sato, Kaoru
    ,
    Shepherd, Theodore G.
    DOI: 10.1175/JAS3800.1
    Publisher: American Meteorological Society
    Abstract: The spatial structure and phase velocity of tropopause disturbances localized around the subpolar jet in the Southern Hemisphere are investigated using 6-hourly European Centre for Medium-Range Weather Forecasts reanalysis data covering 15 yr (1979?93). The phase velocity and phase structure of the tropopause disturbances are in good agreement with those of an edge wave vertically trapped at the tropopause. However, the vertical distribution of the ratio of potential to kinetic energy exhibits maxima above and below the tropopause and a minimum around the tropopause, in contradiction to edge wave theory for which the ratio is unity throughout the troposphere and stratosphere. This difference in vertical structure between the observed tropopause disturbances and edge wave theory is attributed to the effects of a finite-depth tropopause together with the next-order corrections in Rossby number to quasigeostrophic dynamics.
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      A Diagnostic Study of Waves on the Tropopause

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4218381
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    contributor authorTomikawa, Yoshihiro
    contributor authorSato, Kaoru
    contributor authorShepherd, Theodore G.
    date accessioned2017-06-09T16:53:14Z
    date available2017-06-09T16:53:14Z
    date copyright2006/12/01
    date issued2006
    identifier issn0022-4928
    identifier otherams-75985.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218381
    description abstractThe spatial structure and phase velocity of tropopause disturbances localized around the subpolar jet in the Southern Hemisphere are investigated using 6-hourly European Centre for Medium-Range Weather Forecasts reanalysis data covering 15 yr (1979?93). The phase velocity and phase structure of the tropopause disturbances are in good agreement with those of an edge wave vertically trapped at the tropopause. However, the vertical distribution of the ratio of potential to kinetic energy exhibits maxima above and below the tropopause and a minimum around the tropopause, in contradiction to edge wave theory for which the ratio is unity throughout the troposphere and stratosphere. This difference in vertical structure between the observed tropopause disturbances and edge wave theory is attributed to the effects of a finite-depth tropopause together with the next-order corrections in Rossby number to quasigeostrophic dynamics.
    publisherAmerican Meteorological Society
    titleA Diagnostic Study of Waves on the Tropopause
    typeJournal Paper
    journal volume63
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS3800.1
    journal fristpage3315
    journal lastpage3332
    treeJournal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 012
    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