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    Radar Polarimetric Backscattering Properties of Conical Graupel

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 011::page 1887
    Author:
    Aydin, K.
    ,
    Seliga, T. A.
    DOI: 10.1175/1520-0469(1984)041<1887:RPBPOC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Conical graupel is modeled using sphere-cone-oblate spheroidal shapes for the purpose of computing their backscattering properties at a wavelength of 10 cm in terms of the radar polarimetric observables, reflectivity factors, differential reflectivities and circular depolarization ratios. A shape distribution based on in situ measurements is used together with gamma (m=0, 2) size distributions in the computations; both wet and dry graupel are considered. Significant differences in the radar observables between the wet and dry cases are noted and the effects of canting on the radar observables are considered. The implications of these results on the differentiation of hydrometeor phase with radar are discussed.
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      Radar Polarimetric Backscattering Properties of Conical Graupel

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154906
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    contributor authorAydin, K.
    contributor authorSeliga, T. A.
    date accessioned2017-06-09T14:24:57Z
    date available2017-06-09T14:24:57Z
    date copyright1984/06/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18855.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154906
    description abstractConical graupel is modeled using sphere-cone-oblate spheroidal shapes for the purpose of computing their backscattering properties at a wavelength of 10 cm in terms of the radar polarimetric observables, reflectivity factors, differential reflectivities and circular depolarization ratios. A shape distribution based on in situ measurements is used together with gamma (m=0, 2) size distributions in the computations; both wet and dry graupel are considered. Significant differences in the radar observables between the wet and dry cases are noted and the effects of canting on the radar observables are considered. The implications of these results on the differentiation of hydrometeor phase with radar are discussed.
    publisherAmerican Meteorological Society
    titleRadar Polarimetric Backscattering Properties of Conical Graupel
    typeJournal Paper
    journal volume41
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<1887:RPBPOC>2.0.CO;2
    journal fristpage1887
    journal lastpage1892
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;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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