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    Acceleration of the Brewer–Dobson Circulation due to Increases in Greenhouse Gases

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 008::page 2731
    Author:
    Garcia, Rolando R.
    ,
    Randel, William J.
    DOI: 10.1175/2008JAS2712.1
    Publisher: American Meteorological Society
    Abstract: The acceleration of the Brewer?Dobson circulation under rising concentrations of greenhouse gases is investigated using the Whole Atmosphere Community Climate Model. The circulation strengthens as a result of increased wave driving in the subtropical lower stratosphere, which in turn occurs because of enhanced propagation and dissipation of waves in this region. Enhanced wave propagation is due to changes in tropospheric and lower-stratospheric zonal-mean winds, which become more westerly. Ultimately, these trends follow from changes in the zonal-mean temperature distribution caused by the greenhouse effect. The circulation in the middle and upper stratosphere also accelerates as a result of filtering of parameterized gravity waves by stronger subtropical westerly winds.
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      Acceleration of the Brewer–Dobson Circulation due to Increases in Greenhouse Gases

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    contributor authorGarcia, Rolando R.
    contributor authorRandel, William J.
    date accessioned2017-06-09T16:22:54Z
    date available2017-06-09T16:22:54Z
    date copyright2008/08/01
    date issued2008
    identifier issn0022-4928
    identifier otherams-66831.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208210
    description abstractThe acceleration of the Brewer?Dobson circulation under rising concentrations of greenhouse gases is investigated using the Whole Atmosphere Community Climate Model. The circulation strengthens as a result of increased wave driving in the subtropical lower stratosphere, which in turn occurs because of enhanced propagation and dissipation of waves in this region. Enhanced wave propagation is due to changes in tropospheric and lower-stratospheric zonal-mean winds, which become more westerly. Ultimately, these trends follow from changes in the zonal-mean temperature distribution caused by the greenhouse effect. The circulation in the middle and upper stratosphere also accelerates as a result of filtering of parameterized gravity waves by stronger subtropical westerly winds.
    publisherAmerican Meteorological Society
    titleAcceleration of the Brewer–Dobson Circulation due to Increases in Greenhouse Gases
    typeJournal Paper
    journal volume65
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2712.1
    journal fristpage2731
    journal lastpage2739
    treeJournal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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