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    The GISS Global Climate-Middle Atmosphere Model. Part II. Model Variability Due to Interactions between Planetary Waves, the Mean Circulation and Gravity Wave Drag

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 003::page 371
    Author:
    Rind, D.
    ,
    Suozzo, R.
    ,
    Balachandran, N. K.
    DOI: 10.1175/1520-0469(1988)045<0371:TGGCMA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The variability which arises in the GISS Global Climate-Middle Atmosphere Model on two time scales is reviewed: interannual standard deviations, derived from the five-year control run, and intraseasonal variability as exemplifited by stratospheric warmings. The model's extratropical variability for both mean fields and eddy statistics appears reasonable when compared with observations, while the tropical wind variability near the stratopause may be excessive, possibly due to inertial oscillations. Both wave 1 and wave 2 warmings develop, with connections to tropospheric forcing. Variability on both time scales results from a complex set of interactions among planetary waves, the mean circulation, and gravity wave drag. Specific examples of these interactions are presented, which imply that variability in gravity wave forcing and drag may be an important component of the variability of the middle atmosphere.
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      The GISS Global Climate-Middle Atmosphere Model. Part II. Model Variability Due to Interactions between Planetary Waves, the Mean Circulation and Gravity Wave Drag

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155888
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    • Journal of the Atmospheric Sciences

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    contributor authorRind, D.
    contributor authorSuozzo, R.
    contributor authorBalachandran, N. K.
    date accessioned2017-06-09T14:28:00Z
    date available2017-06-09T14:28:00Z
    date copyright1988/02/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19739.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155888
    description abstractThe variability which arises in the GISS Global Climate-Middle Atmosphere Model on two time scales is reviewed: interannual standard deviations, derived from the five-year control run, and intraseasonal variability as exemplifited by stratospheric warmings. The model's extratropical variability for both mean fields and eddy statistics appears reasonable when compared with observations, while the tropical wind variability near the stratopause may be excessive, possibly due to inertial oscillations. Both wave 1 and wave 2 warmings develop, with connections to tropospheric forcing. Variability on both time scales results from a complex set of interactions among planetary waves, the mean circulation, and gravity wave drag. Specific examples of these interactions are presented, which imply that variability in gravity wave forcing and drag may be an important component of the variability of the middle atmosphere.
    publisherAmerican Meteorological Society
    titleThe GISS Global Climate-Middle Atmosphere Model. Part II. Model Variability Due to Interactions between Planetary Waves, the Mean Circulation and Gravity Wave Drag
    typeJournal Paper
    journal volume45
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<0371:TGGCMA>2.0.CO;2
    journal fristpage371
    journal lastpage386
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;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