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    The Quasi-biennial Oscillation of Ozone in the Tropical Middle Stratosphere: A One-Dimensional Model

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 024::page 3122
    Author:
    Ling, Xiu-De
    ,
    London, Julius
    DOI: 10.1175/1520-0469(1986)043<3122:TQBOOO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A one-dimensional model of the quasi-biennial oscillation (QBO) of ozone in the tropical middle stratosphere is derived based on assumed (observed) zonal wind QBO in a coupled dynamic, radiative/ photochemical system. It is found that the derived vertical variation of the ozone QBO amplitude has two. maxima, one at 32 km and the other at 22 km, and a minimum at 28 km. These are in qualitative agreement with observations. In the height interval 30?35 km, the ozone QBO is closely related to temperature dependent photochemistry and the ozone and temperature variations are out of phase. Below 28 km, where vertical ozone and thermal transports are important, ozone and temperature oscillations are in phase but both am approximately 270° out of phase with the vertical wind variation.
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      The Quasi-biennial Oscillation of Ozone in the Tropical Middle Stratosphere: A One-Dimensional Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155546
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    contributor authorLing, Xiu-De
    contributor authorLondon, Julius
    date accessioned2017-06-09T14:26:56Z
    date available2017-06-09T14:26:56Z
    date copyright1986/12/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19430.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155546
    description abstractA one-dimensional model of the quasi-biennial oscillation (QBO) of ozone in the tropical middle stratosphere is derived based on assumed (observed) zonal wind QBO in a coupled dynamic, radiative/ photochemical system. It is found that the derived vertical variation of the ozone QBO amplitude has two. maxima, one at 32 km and the other at 22 km, and a minimum at 28 km. These are in qualitative agreement with observations. In the height interval 30?35 km, the ozone QBO is closely related to temperature dependent photochemistry and the ozone and temperature variations are out of phase. Below 28 km, where vertical ozone and thermal transports are important, ozone and temperature oscillations are in phase but both am approximately 270° out of phase with the vertical wind variation.
    publisherAmerican Meteorological Society
    titleThe Quasi-biennial Oscillation of Ozone in the Tropical Middle Stratosphere: A One-Dimensional Model
    typeJournal Paper
    journal volume43
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<3122:TQBOOO>2.0.CO;2
    journal fristpage3122
    journal lastpage3137
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 024
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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