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    Structures of Bragg Scatter Observed with the Polarimetric WSR-88D

    Source: Journal of Atmospheric and Oceanic Technology:;2013:;volume( 030 ):;issue: 007::page 1253
    Author:
    Melnikov, Valery M.
    ,
    Doviak, Richard J.
    ,
    Zrnić, Dusan S.
    ,
    Stensrud, David J.
    DOI: 10.1175/JTECH-D-12-00210.1
    Publisher: American Meteorological Society
    Abstract: nhancements to signal processing and data collection in the dual-polarization Weather Surveillance Radar-1988 Doppler (WSR-88D) to increase its detection capability yield observations of ?fine? structures from Bragg scatterers. Several types of the fine structures observed in and above the boundary layer are discussed. These Bragg scatter structures include the top of the convective boundary layer, nonprecipitating clouds, strong convective plumes above the boundary layer, and a layer of weak reflections associated with decaying boundary layer turbulence. A conclusion that data from polarimetric WSR-88Ds can be used to obtain the depth of the convective boundary layer is made.
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      Structures of Bragg Scatter Observed with the Polarimetric WSR-88D

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4228197
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    contributor authorMelnikov, Valery M.
    contributor authorDoviak, Richard J.
    contributor authorZrnić, Dusan S.
    contributor authorStensrud, David J.
    date accessioned2017-06-09T17:24:58Z
    date available2017-06-09T17:24:58Z
    date copyright2013/07/01
    date issued2013
    identifier issn0739-0572
    identifier otherams-84819.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228197
    description abstractnhancements to signal processing and data collection in the dual-polarization Weather Surveillance Radar-1988 Doppler (WSR-88D) to increase its detection capability yield observations of ?fine? structures from Bragg scatterers. Several types of the fine structures observed in and above the boundary layer are discussed. These Bragg scatter structures include the top of the convective boundary layer, nonprecipitating clouds, strong convective plumes above the boundary layer, and a layer of weak reflections associated with decaying boundary layer turbulence. A conclusion that data from polarimetric WSR-88Ds can be used to obtain the depth of the convective boundary layer is made.
    publisherAmerican Meteorological Society
    titleStructures of Bragg Scatter Observed with the Polarimetric WSR-88D
    typeJournal Paper
    journal volume30
    journal issue7
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH-D-12-00210.1
    journal fristpage1253
    journal lastpage1258
    treeJournal of Atmospheric and Oceanic Technology:;2013:;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
    yabeshDSpacePersian