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    Attenuation Correction in Dual-Wavelength Analyses

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 011::page 1914
    Author:
    Tuttle, John D.
    ,
    Rinehart, Ronald E.
    DOI: 10.1175/1520-0450(1983)022<1914:ACIDWA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In using a dual-wavelength radar system to detect hail, erroneous positive hail signals can result because of the stronger attenuation of the shorter wavelength radar beam. We present a simple technique to correct for attenuation in dual-wavelength analyses. The technique makes use of an attenuation-reflectivity relationship of the form, A = CZxp, where Zx is the S-band reflectivity, C is a coefficient which is determined on a ray-by-ray basis, and p is the exponent, which is assumed to be a constant. In situations where rays of radar data contain a mixture of rain and hail, the attenuation-correction scheme can erroneously apportion more of the attenuation to hail regions rather than to rain regions. The scheme is modified to account for such situations.
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      Attenuation Correction in Dual-Wavelength Analyses

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145749
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    • Journal of Climate and Applied Meteorology

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    contributor authorTuttle, John D.
    contributor authorRinehart, Ronald E.
    date accessioned2017-06-09T13:59:51Z
    date available2017-06-09T13:59:51Z
    date copyright1983/11/01
    date issued1983
    identifier issn0733-3021
    identifier otherams-10612.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145749
    description abstractIn using a dual-wavelength radar system to detect hail, erroneous positive hail signals can result because of the stronger attenuation of the shorter wavelength radar beam. We present a simple technique to correct for attenuation in dual-wavelength analyses. The technique makes use of an attenuation-reflectivity relationship of the form, A = CZxp, where Zx is the S-band reflectivity, C is a coefficient which is determined on a ray-by-ray basis, and p is the exponent, which is assumed to be a constant. In situations where rays of radar data contain a mixture of rain and hail, the attenuation-correction scheme can erroneously apportion more of the attenuation to hail regions rather than to rain regions. The scheme is modified to account for such situations.
    publisherAmerican Meteorological Society
    titleAttenuation Correction in Dual-Wavelength Analyses
    typeJournal Paper
    journal volume22
    journal issue11
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1983)022<1914:ACIDWA>2.0.CO;2
    journal fristpage1914
    journal lastpage1921
    treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 011
    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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