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    The 26-Month Oscillation in Zonal Wind and Temperature

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 006::page 786
    Author:
    Shah, G. M.
    ,
    Godson, W. L.
    DOI: 10.1175/1520-0469(1966)023<0786:TMOIZW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Harmonic analysis of mean monthly zonal wind and temperature data,after removing the annual cycle, have shown the existence of the 26-month oscillation in the equatorial stratosphere. The oscillation in temperature extends to temperate and polar latitudes, while in zonal wind it is insignificant beyond 25N. The amplitude of the 26-month oscillation in temperature follows a meridional wave pattern with an approximate wavelength of about 30 deg of latitude. The phase of the 26-month oscillation in both zonal wind and temperature progresses downward, at equatorial latitudes, with a speed a little less than 1 km per month. The oscillation in temperature at the position of the tropical amplitude maximum is approximately out of phase with the oscillations at high level equatorial latitudes and at temperate and polar latitudes.
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      The 26-Month Oscillation in Zonal Wind and Temperature

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4150921
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    contributor authorShah, G. M.
    contributor authorGodson, W. L.
    date accessioned2017-06-09T14:13:58Z
    date available2017-06-09T14:13:58Z
    date copyright1966/11/01
    date issued1966
    identifier issn0022-4928
    identifier otherams-15268.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150921
    description abstractHarmonic analysis of mean monthly zonal wind and temperature data,after removing the annual cycle, have shown the existence of the 26-month oscillation in the equatorial stratosphere. The oscillation in temperature extends to temperate and polar latitudes, while in zonal wind it is insignificant beyond 25N. The amplitude of the 26-month oscillation in temperature follows a meridional wave pattern with an approximate wavelength of about 30 deg of latitude. The phase of the 26-month oscillation in both zonal wind and temperature progresses downward, at equatorial latitudes, with a speed a little less than 1 km per month. The oscillation in temperature at the position of the tropical amplitude maximum is approximately out of phase with the oscillations at high level equatorial latitudes and at temperate and polar latitudes.
    publisherAmerican Meteorological Society
    titleThe 26-Month Oscillation in Zonal Wind and Temperature
    typeJournal Paper
    journal volume23
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1966)023<0786:TMOIZW>2.0.CO;2
    journal fristpage786
    journal lastpage790
    treeJournal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 006
    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