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    Dispersion and Spectra of Gravity Waves in the Atmosphere

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 006::page 1540
    Author:
    Gossard, E. E.
    ,
    Sweezy, W. B.
    DOI: 10.1175/1520-0469(1974)031<1540:DASOGW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper describes a method for obtaining the dispersion properties of atmospheric waves from ground-based measurements of pressure and wind fluctuations. Having found the wave dispersion, we can find the displacement spectra of the waves aloft, making only minimal assumptions about the atmospheric model and, without having very accurate sounding information. We have applied the method to a pair of events for which we had fairly complete documentation. In one case, the waves aloft were observed with a vertically-pointing, high-resolution FM-CW radar, and we have compared the observed vertical displacement spectra with those deduced from ground measurements. In another case, the waves were associated with a weather front and a nearby tropical storm. The ground measurements permitted us to deduce the history of the waves aloft, and we found that the wave system before passage of the front differed dramatically from the waves present after frontal passage.
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      Dispersion and Spectra of Gravity Waves in the Atmosphere

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152429
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    contributor authorGossard, E. E.
    contributor authorSweezy, W. B.
    date accessioned2017-06-09T14:17:39Z
    date available2017-06-09T14:17:39Z
    date copyright1974/09/01
    date issued1974
    identifier issn0022-4928
    identifier otherams-16625.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152429
    description abstractThis paper describes a method for obtaining the dispersion properties of atmospheric waves from ground-based measurements of pressure and wind fluctuations. Having found the wave dispersion, we can find the displacement spectra of the waves aloft, making only minimal assumptions about the atmospheric model and, without having very accurate sounding information. We have applied the method to a pair of events for which we had fairly complete documentation. In one case, the waves aloft were observed with a vertically-pointing, high-resolution FM-CW radar, and we have compared the observed vertical displacement spectra with those deduced from ground measurements. In another case, the waves were associated with a weather front and a nearby tropical storm. The ground measurements permitted us to deduce the history of the waves aloft, and we found that the wave system before passage of the front differed dramatically from the waves present after frontal passage.
    publisherAmerican Meteorological Society
    titleDispersion and Spectra of Gravity Waves in the Atmosphere
    typeJournal Paper
    journal volume31
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1974)031<1540:DASOGW>2.0.CO;2
    journal fristpage1540
    journal lastpage1548
    treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 006
    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
    yabeshDSpacePersian