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    Winds and Wave Motions to 110 km at Mid-Latitudes. III. Response of Mesospheric and Thermospheric Winds to Major Stratospheric Warmings

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 009::page 1676
    Author:
    Gregory, J. B.
    ,
    Manson, A. H.
    DOI: 10.1175/1520-0469(1975)032<1676:WAWMTK>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The behavior of winds at 52°N, 107°W (Saskatoon, Canada) at altitudes to ?110 km during major stratospheric warmings of 1969?70,1970?-71 and 1972?73 winters and a minor warming in December 1972, is studied. The zonal component of flow above the stratosphere is found to be affected to varying altitudes; in January 1970 the normal eastward flow was reversed to westward at all altitudes from the surface to ?110 km. The pattern of winds is reasonably consistent with current suggestions that at middle and high latitudes the mesosphere cools as the stratosphere warms, and that the mesosphere warms subsequent to its cooling. Examples of mesospheric wind perturbations either as precursors of stratospheric warmings or independent of warmings, are also given.
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      Winds and Wave Motions to 110 km at Mid-Latitudes. III. Response of Mesospheric and Thermospheric Winds to Major Stratospheric Warmings

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4152730
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    • Journal of the Atmospheric Sciences

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    contributor authorGregory, J. B.
    contributor authorManson, A. H.
    date accessioned2017-06-09T14:18:24Z
    date available2017-06-09T14:18:24Z
    date copyright1975/09/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16897.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152730
    description abstractThe behavior of winds at 52°N, 107°W (Saskatoon, Canada) at altitudes to ?110 km during major stratospheric warmings of 1969?70,1970?-71 and 1972?73 winters and a minor warming in December 1972, is studied. The zonal component of flow above the stratosphere is found to be affected to varying altitudes; in January 1970 the normal eastward flow was reversed to westward at all altitudes from the surface to ?110 km. The pattern of winds is reasonably consistent with current suggestions that at middle and high latitudes the mesosphere cools as the stratosphere warms, and that the mesosphere warms subsequent to its cooling. Examples of mesospheric wind perturbations either as precursors of stratospheric warmings or independent of warmings, are also given.
    publisherAmerican Meteorological Society
    titleWinds and Wave Motions to 110 km at Mid-Latitudes. III. Response of Mesospheric and Thermospheric Winds to Major Stratospheric Warmings
    typeJournal Paper
    journal volume32
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<1676:WAWMTK>2.0.CO;2
    journal fristpage1676
    journal lastpage1682
    treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;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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