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    Automatic Detection of Gust Fronts

    Source: Journal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 001::page 36
    Author:
    Uyeda, Hiroshi
    ,
    Zrnić, Dusan S.
    DOI: 10.1175/1520-0426(1986)003<0036:ADOGF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We have developed a procedure that detects and tracks gust fronts automatically. It does not rely on a single method but requires simultaneous operation of two related algorithms. The convergence algorithm measures radial convergence and hence only gusts propagating along radials can be readily detected. The mesocyclone-shear algorithm measures azimuthal shear and is suitable for detecting gusts parallel with radials as well as low-level vortices. Long shear lines that these algorithms detect are classified as gusts whereas symmetric shear features are rejected if their shear and flux or ?momentum? are insignificant; otherwise they are classified as low-level vortices. To locate gusts we use second-order polynomials in the range-azimuth plane. It is shown that predicted gust locations from simple linear projections of the least square fitted curves agree very well with actual gust locations.
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      Automatic Detection of Gust Fronts

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153178
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorUyeda, Hiroshi
    contributor authorZrnić, Dusan S.
    date accessioned2017-06-09T14:19:33Z
    date available2017-06-09T14:19:33Z
    date copyright1986/03/01
    date issued1986
    identifier issn0739-0572
    identifier otherams-173.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153178
    description abstractWe have developed a procedure that detects and tracks gust fronts automatically. It does not rely on a single method but requires simultaneous operation of two related algorithms. The convergence algorithm measures radial convergence and hence only gusts propagating along radials can be readily detected. The mesocyclone-shear algorithm measures azimuthal shear and is suitable for detecting gusts parallel with radials as well as low-level vortices. Long shear lines that these algorithms detect are classified as gusts whereas symmetric shear features are rejected if their shear and flux or ?momentum? are insignificant; otherwise they are classified as low-level vortices. To locate gusts we use second-order polynomials in the range-azimuth plane. It is shown that predicted gust locations from simple linear projections of the least square fitted curves agree very well with actual gust locations.
    publisherAmerican Meteorological Society
    titleAutomatic Detection of Gust Fronts
    typeJournal Paper
    journal volume3
    journal issue1
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1986)003<0036:ADOGF>2.0.CO;2
    journal fristpage36
    journal lastpage50
    treeJournal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 001
    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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