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    NOTE ON THE SEMI-ANNUAL WIND VARIATION IN THE EQUATORIAL STRATOSPHERE

    Source: Monthly Weather Review:;1967:;volume( 095 ):;issue: 009::page 635
    Author:
    QUIROZ, RODERICK S.
    ,
    MILLER, ALVIN J.
    DOI: 10.1175/1520-0493(1967)095<0635:NOTSAW>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: Rocket wind soundings for several stations within 10° latitude of the equator are used to analyze details of the structure of the recently discovered semi-annual wind variation in the equatorial upper stratosphere. The cycle is characterized by winter and summer easterlies and equinoctial westerlies and in 1966 appeared to have maximum amplitude at 45?50 km. Its global extent is confirmed with the aid of rocket data from widely separated longitudes. The semi-annual variation is discussed in relation to the quasi-biennial oscillation, which has maximum amplitude in the lower stratosphere. A possible explanation of the origin of the semi-annual variation is mentioned and attention is called to semi-annual variations in other parameters in the upper atmosphere.
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      NOTE ON THE SEMI-ANNUAL WIND VARIATION IN THE EQUATORIAL STRATOSPHERE

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4198265
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    • Monthly Weather Review

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    contributor authorQUIROZ, RODERICK S.
    contributor authorMILLER, ALVIN J.
    date accessioned2017-06-09T15:58:30Z
    date available2017-06-09T15:58:30Z
    date copyright1967/09/01
    date issued1967
    identifier issn0027-0644
    identifier otherams-57881.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198265
    description abstractRocket wind soundings for several stations within 10° latitude of the equator are used to analyze details of the structure of the recently discovered semi-annual wind variation in the equatorial upper stratosphere. The cycle is characterized by winter and summer easterlies and equinoctial westerlies and in 1966 appeared to have maximum amplitude at 45?50 km. Its global extent is confirmed with the aid of rocket data from widely separated longitudes. The semi-annual variation is discussed in relation to the quasi-biennial oscillation, which has maximum amplitude in the lower stratosphere. A possible explanation of the origin of the semi-annual variation is mentioned and attention is called to semi-annual variations in other parameters in the upper atmosphere.
    publisherAmerican Meteorological Society
    titleNOTE ON THE SEMI-ANNUAL WIND VARIATION IN THE EQUATORIAL STRATOSPHERE
    typeJournal Paper
    journal volume95
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1967)095<0635:NOTSAW>2.3.CO;2
    journal fristpage635
    journal lastpage641
    treeMonthly Weather Review:;1967:;volume( 095 ):;issue: 009
    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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