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    Tropical Intraseasonal Oscillations Appearing in a GFDL General Circulation Model and FGGE Data. Part II: Structure

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 021::page 3017
    Author:
    Hayashi, Y.
    ,
    Golder, D. G.
    DOI: 10.1175/1520-0469(1988)045<3017:TIOAIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Space-time spectral and filter analyses are made of the structure of the tropical intraseasonal oscillations appearing in a GFDL 30-wavenumber spectral general circulation model and the FGGE IIIb data set. The model's tropical zonal velocity exhibits spectral peaks with periods of 40?50 and 25?30 days at wavenumber 1 for six individual years, although the 40?50 day peak is not as pronounced as that found in the FGGE dataset. Both the eastward moving 40?50 and 25?30 day oscillations take the form of a Kelvin?Rossby wave pattern in the upper troposphere and a Rossby mode in the lower troposphere. They also take the form of a latitudinally tilted Walker cell which is modified by a meridional convergence in the boundary layer.
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      Tropical Intraseasonal Oscillations Appearing in a GFDL General Circulation Model and FGGE Data. Part II: Structure

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156080
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    contributor authorHayashi, Y.
    contributor authorGolder, D. G.
    date accessioned2017-06-09T14:28:29Z
    date available2017-06-09T14:28:29Z
    date copyright1988/11/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19911.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156080
    description abstractSpace-time spectral and filter analyses are made of the structure of the tropical intraseasonal oscillations appearing in a GFDL 30-wavenumber spectral general circulation model and the FGGE IIIb data set. The model's tropical zonal velocity exhibits spectral peaks with periods of 40?50 and 25?30 days at wavenumber 1 for six individual years, although the 40?50 day peak is not as pronounced as that found in the FGGE dataset. Both the eastward moving 40?50 and 25?30 day oscillations take the form of a Kelvin?Rossby wave pattern in the upper troposphere and a Rossby mode in the lower troposphere. They also take the form of a latitudinally tilted Walker cell which is modified by a meridional convergence in the boundary layer.
    publisherAmerican Meteorological Society
    titleTropical Intraseasonal Oscillations Appearing in a GFDL General Circulation Model and FGGE Data. Part II: Structure
    typeJournal Paper
    journal volume45
    journal issue21
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<3017:TIOAIA>2.0.CO;2
    journal fristpage3017
    journal lastpage3033
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 021
    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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