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    The Tropical Semiannual Oscillations in Temperature and Ozone as Observed by the MLS

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 020::page 3045
    Author:
    Ray, Eric A.
    ,
    Holton, James R.
    ,
    Fishbein, Evan F.
    ,
    Froidevaux, Lucien
    ,
    Waters, J. W.
    DOI: 10.1175/1520-0469(1994)051<3045:TTSOIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The first two years of MLS temperature and ozone data are used to examine the tropical upper-stratospheric SAO. Time series analysis revealed that the strongest amplitudes of the SAO occurred near the equator at 2 mb for temperature and 5 mb for ozone, consistent with previous observations. The first cycle of each calendar year was observed to have a much higher amplitude than the second cycle except for the warm phase in late 1991. Interannual variability in the strength of the SAO, such as the much stronger warm phase of late 1991 as compared to late 1992, was significant and could be partly attributed to the QBO in zonal wind.
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      The Tropical Semiannual Oscillations in Temperature and Ozone as Observed by the MLS

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4157617
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    • Journal of the Atmospheric Sciences

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    contributor authorRay, Eric A.
    contributor authorHolton, James R.
    contributor authorFishbein, Evan F.
    contributor authorFroidevaux, Lucien
    contributor authorWaters, J. W.
    date accessioned2017-06-09T14:32:33Z
    date available2017-06-09T14:32:33Z
    date copyright1994/10/01
    date issued1994
    identifier issn0022-4928
    identifier otherams-21294.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157617
    description abstractThe first two years of MLS temperature and ozone data are used to examine the tropical upper-stratospheric SAO. Time series analysis revealed that the strongest amplitudes of the SAO occurred near the equator at 2 mb for temperature and 5 mb for ozone, consistent with previous observations. The first cycle of each calendar year was observed to have a much higher amplitude than the second cycle except for the warm phase in late 1991. Interannual variability in the strength of the SAO, such as the much stronger warm phase of late 1991 as compared to late 1992, was significant and could be partly attributed to the QBO in zonal wind.
    publisherAmerican Meteorological Society
    titleThe Tropical Semiannual Oscillations in Temperature and Ozone as Observed by the MLS
    typeJournal Paper
    journal volume51
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1994)051<3045:TTSOIT>2.0.CO;2
    journal fristpage3045
    journal lastpage3052
    treeJournal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 020
    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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