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    On the Sensitivity of Annular Mode Dynamics to Stratospheric Radiative Time Scales

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 002::page 476
    Author:
    Charlton-Perez, Andrew J.
    ,
    O’Neill, Alan
    DOI: 10.1175/2009JCLI2995.1
    Publisher: American Meteorological Society
    Abstract: Long decorrelation time scales of the annular mode are observed in the lower stratosphere. This study uses a simple dynamical model, which has been used extensively to study stratosphere?troposphere coupling to investigate the origin of the long dynamical time scales. Several long runs of the model are completed, with different imposed thermal damping time scales in the stratosphere. The dynamical time scales of the annular mode are found to be largely insensitive to the input thermal damping time scales, producing similar dynamical time scales in all cases below 50 hPa. This result suggests that the hypothesis that long time scales in the lower stratosphere are due to long radiative time scales in this region is false.
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      On the Sensitivity of Annular Mode Dynamics to Stratospheric Radiative Time Scales

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210446
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    contributor authorCharlton-Perez, Andrew J.
    contributor authorO’Neill, Alan
    date accessioned2017-06-09T16:29:34Z
    date available2017-06-09T16:29:34Z
    date copyright2010/01/01
    date issued2010
    identifier issn0894-8755
    identifier otherams-68843.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210446
    description abstractLong decorrelation time scales of the annular mode are observed in the lower stratosphere. This study uses a simple dynamical model, which has been used extensively to study stratosphere?troposphere coupling to investigate the origin of the long dynamical time scales. Several long runs of the model are completed, with different imposed thermal damping time scales in the stratosphere. The dynamical time scales of the annular mode are found to be largely insensitive to the input thermal damping time scales, producing similar dynamical time scales in all cases below 50 hPa. This result suggests that the hypothesis that long time scales in the lower stratosphere are due to long radiative time scales in this region is false.
    publisherAmerican Meteorological Society
    titleOn the Sensitivity of Annular Mode Dynamics to Stratospheric Radiative Time Scales
    typeJournal Paper
    journal volume23
    journal issue2
    journal titleJournal of Climate
    identifier doi10.1175/2009JCLI2995.1
    journal fristpage476
    journal lastpage484
    treeJournal of Climate:;2010:;volume( 023 ):;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
    yabeshDSpacePersian