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    Wind Oscillations Between 30 and 60 km Over White Sands Missile Range, New Mexico

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 004::page 382
    Author:
    Miers, Bruce T.
    DOI: 10.1175/1520-0469(1965)022<0382:WOBAKO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Analyses of three series of meteorological rocket soundings have indicated diurnal and semidiurnal cycles in the winds between 30 and 60 km. Each series comprised a one day sample with the soundings over White Sands Missile Range taken on 7?8 February 1964 and 21?22 November 1964 being compared with the sounding taken over Eglin AFB, Florida on 9?10 May 1961. In general the winds turned clockwise for the periods of time examined, indicating a diurnal cycle in the wind field. In most cases the amplitude of the diurnal component was larger than the amplitude of the semidiurnal component, with the diurnal component undergoing systematic fluctuations with height. It was found that the diurnal and semidiurnal oscillations were not uniform, but occurred in layers of strong and weak oscillations with different phases in the different layers. The largest amplitudes occurred at 45 km where the heating of the ozone by solar ultraviolet is a maximum.
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      Wind Oscillations Between 30 and 60 km Over White Sands Missile Range, New Mexico

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    contributor authorMiers, Bruce T.
    date accessioned2017-06-09T14:13:33Z
    date available2017-06-09T14:13:33Z
    date copyright1965/07/01
    date issued1965
    identifier issn0022-4928
    identifier otherams-15107.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150743
    description abstractAnalyses of three series of meteorological rocket soundings have indicated diurnal and semidiurnal cycles in the winds between 30 and 60 km. Each series comprised a one day sample with the soundings over White Sands Missile Range taken on 7?8 February 1964 and 21?22 November 1964 being compared with the sounding taken over Eglin AFB, Florida on 9?10 May 1961. In general the winds turned clockwise for the periods of time examined, indicating a diurnal cycle in the wind field. In most cases the amplitude of the diurnal component was larger than the amplitude of the semidiurnal component, with the diurnal component undergoing systematic fluctuations with height. It was found that the diurnal and semidiurnal oscillations were not uniform, but occurred in layers of strong and weak oscillations with different phases in the different layers. The largest amplitudes occurred at 45 km where the heating of the ozone by solar ultraviolet is a maximum.
    publisherAmerican Meteorological Society
    titleWind Oscillations Between 30 and 60 km Over White Sands Missile Range, New Mexico
    typeJournal Paper
    journal volume22
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1965)022<0382:WOBAKO>2.0.CO;2
    journal fristpage382
    journal lastpage387
    treeJournal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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