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    Wind Gradients and Variance of Doppler Spectra in Showers Viewed Horizontally

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 004::page 688
    Author:
    Battan, Louis J.
    ,
    Theiss, John B.
    DOI: 10.1175/1520-0450(1973)012<0688:WGAVOD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An X-band pulsed-Doppler radar having its beam fixed at an elevation angle of 3°, has supplied new data on radial velocity spectra in two showers. It was found that the mean Doppler velocity, variance of the Doppler spectrum, and radar reflectivity varied markedly over distances of less than a kilometer. The observed variances were less than about 1 m2 sec?2 in more than 80% of the observations and exceeded 3 m2 sec?2 in about 4% of the cases. An analysis of ?V?/?r, the radial gradient of the mean Doppler velocity, yielded a nearly Gaussian curve having a mean of 0.2 ? 10?2 sec?1 and a standard deviation of 5.8 ? 10?3 sec?1. The effects of the radial gradient of the radial wind apparently can explain less than about 15% of the observed variance of the Doppler spectrum. It appears that a major part of the variance is attributable to scales of motion smaller than the dimensions of the sampling volume.
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      Wind Gradients and Variance of Doppler Spectra in Showers Viewed Horizontally

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4229155
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    contributor authorBattan, Louis J.
    contributor authorTheiss, John B.
    date accessioned2017-06-09T17:27:44Z
    date available2017-06-09T17:27:44Z
    date copyright1973/06/01
    date issued1973
    identifier issn0021-8952
    identifier otherams-8568.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229155
    description abstractAn X-band pulsed-Doppler radar having its beam fixed at an elevation angle of 3°, has supplied new data on radial velocity spectra in two showers. It was found that the mean Doppler velocity, variance of the Doppler spectrum, and radar reflectivity varied markedly over distances of less than a kilometer. The observed variances were less than about 1 m2 sec?2 in more than 80% of the observations and exceeded 3 m2 sec?2 in about 4% of the cases. An analysis of ?V?/?r, the radial gradient of the mean Doppler velocity, yielded a nearly Gaussian curve having a mean of 0.2 ? 10?2 sec?1 and a standard deviation of 5.8 ? 10?3 sec?1. The effects of the radial gradient of the radial wind apparently can explain less than about 15% of the observed variance of the Doppler spectrum. It appears that a major part of the variance is attributable to scales of motion smaller than the dimensions of the sampling volume.
    publisherAmerican Meteorological Society
    titleWind Gradients and Variance of Doppler Spectra in Showers Viewed Horizontally
    typeJournal Paper
    journal volume12
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1973)012<0688:WGAVOD>2.0.CO;2
    journal fristpage688
    journal lastpage693
    treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 004
    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