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    Winds and Wave Motions to 110 km at Mid-Latitudes. IV. Coupling Between Internal Gravity Waves and the Mean Flow

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 009::page 1682
    Author:
    Manson, A. H.
    ,
    Gregory, J. B.
    ,
    Stephenson, D. G.
    DOI: 10.1175/1520-0469(1975)032<1682:WAWMTK>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The results of radiowave, partial reflection drift (wind) measurements from 60?110 km, for the years 1973?74, at Saskatoon, Canada (52°N, 107°W), are presented. Intensive soundings (12 profiles per hour) have provided hourly, weekly and monthly profiles for the prevailing winds and also for the amplitudes of internal gravity (I.G.) waves (τ≈60 min). A relationship between the heights of reversals of the mean flow and of maxima in the I. G. wave amplitude profiles is demonstrated for 1973 and 1974. Hourly changes in the flow are also shown to be consistent with the effects of longer period (τ≈120 min) I. G. waves and/or momentum deposition by I. G. waves (τ?60 min). It is shown that gravity waves are a major contribution to the dynamical and energetic balance of the lower thermosphere (80?110 km).
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      Winds and Wave Motions to 110 km at Mid-Latitudes. IV. Coupling Between Internal Gravity Waves and the Mean Flow

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4152731
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    • Journal of the Atmospheric Sciences

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    contributor authorManson, A. H.
    contributor authorGregory, J. B.
    contributor authorStephenson, D. G.
    date accessioned2017-06-09T14:18:24Z
    date available2017-06-09T14:18:24Z
    date copyright1975/09/01
    date issued1975
    identifier issn0022-4928
    identifier otherams-16898.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152731
    description abstractThe results of radiowave, partial reflection drift (wind) measurements from 60?110 km, for the years 1973?74, at Saskatoon, Canada (52°N, 107°W), are presented. Intensive soundings (12 profiles per hour) have provided hourly, weekly and monthly profiles for the prevailing winds and also for the amplitudes of internal gravity (I.G.) waves (τ≈60 min). A relationship between the heights of reversals of the mean flow and of maxima in the I. G. wave amplitude profiles is demonstrated for 1973 and 1974. Hourly changes in the flow are also shown to be consistent with the effects of longer period (τ≈120 min) I. G. waves and/or momentum deposition by I. G. waves (τ?60 min). It is shown that gravity waves are a major contribution to the dynamical and energetic balance of the lower thermosphere (80?110 km).
    publisherAmerican Meteorological Society
    titleWinds and Wave Motions to 110 km at Mid-Latitudes. IV. Coupling Between Internal Gravity Waves and the Mean Flow
    typeJournal Paper
    journal volume32
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1975)032<1682:WAWMTK>2.0.CO;2
    journal fristpage1682
    journal lastpage1688
    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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