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    Upper Atmospheric Planetary-Wave and Gravity-Wave Observations

    Source: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007::page 1267
    Author:
    Justus, C. G.
    ,
    Woodrum, Arthur
    DOI: 10.1175/1520-0469(1973)030<1267:UAPWAG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Previously collected data on atmospheric pressure, density, temperature and winds between 25 and 200 km from sources including Meteorological Rocket Network data, ROBIN falling sphere data, grenade release and pitot tube data, meteor winds, chemical release winds, satellite data, and others were analysed by a daily-difference method, and results on the magnitude of atmospheric perturbations interpreted as gravity waves and planetary waves are presented. Traveling planetary-wave contributions in the 25?85 km range were found to have a significant height and latitudinal variation. It was found that observed gravity-wave density perturbations and wind are related to one another in the manner predicted by gravity-wave theory. It was determined that, on the average, gravity-wave energy deposition or reflection occurs at all altitudes except the 55?75 km region of the mesosphere.
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      Upper Atmospheric Planetary-Wave and Gravity-Wave Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152222
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    contributor authorJustus, C. G.
    contributor authorWoodrum, Arthur
    date accessioned2017-06-09T14:17:10Z
    date available2017-06-09T14:17:10Z
    date copyright1973/10/01
    date issued1973
    identifier issn0022-4928
    identifier otherams-16439.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152222
    description abstractPreviously collected data on atmospheric pressure, density, temperature and winds between 25 and 200 km from sources including Meteorological Rocket Network data, ROBIN falling sphere data, grenade release and pitot tube data, meteor winds, chemical release winds, satellite data, and others were analysed by a daily-difference method, and results on the magnitude of atmospheric perturbations interpreted as gravity waves and planetary waves are presented. Traveling planetary-wave contributions in the 25?85 km range were found to have a significant height and latitudinal variation. It was found that observed gravity-wave density perturbations and wind are related to one another in the manner predicted by gravity-wave theory. It was determined that, on the average, gravity-wave energy deposition or reflection occurs at all altitudes except the 55?75 km region of the mesosphere.
    publisherAmerican Meteorological Society
    titleUpper Atmospheric Planetary-Wave and Gravity-Wave Observations
    typeJournal Paper
    journal volume30
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1973)030<1267:UAPWAG>2.0.CO;2
    journal fristpage1267
    journal lastpage1275
    treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007
    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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