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    Can a Unique Model Describe the Raindrop Shape–Size Relation? A Clue from Polarimetric Radar Measurements

    Source: Journal of Atmospheric and Oceanic Technology:;2009:;volume( 026 ):;issue: 009::page 1829
    Author:
    Gorgucci, Eugenio
    ,
    Chandrasekar, V.
    ,
    Baldini, Luca
    DOI: 10.1175/2009JTECHA1183.1
    Publisher: American Meteorological Society
    Abstract: A method is proposed to retrieve raindrop shape?size relations from the radar measurements of reflectivity factor Zh, differential reflectivity Zdr, and specific differential phase Kdp at S band. This procedure is obtained using a domain defined by the two variables Kdp/Zh and Zdr where the drop size distribution (DSD) variability is collapsed onto a line and any variation is essentially due to the drop shape variability. To obtain information on the raindrop shape?size relation underlying a set of radar observations, this domain is studied in conjunction with another domain describing the relation between the drop axial ratio (or shape) and its equivolumetric diameter. Using an initial drop shape and choosing a set of DSDs described by a normalized gamma model, polarimetric radar measurements are produced by simulation. An averaged curve of Kdp/Zh versus Zdr is obtained and compared with the same curve obtained from the radar data. By changing the initial axial ratio relation, a procedure of minimization between the two curves is developed to derive the underlying drop shape?size relation governing the radar measurements under consideration. Three sets of radar data collected in different climatic regions are analyzed to evaluate whether there is a unique shape?size relation.
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      Can a Unique Model Describe the Raindrop Shape–Size Relation? A Clue from Polarimetric Radar Measurements

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4210927
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    contributor authorGorgucci, Eugenio
    contributor authorChandrasekar, V.
    contributor authorBaldini, Luca
    date accessioned2017-06-09T16:31:06Z
    date available2017-06-09T16:31:06Z
    date copyright2009/09/01
    date issued2009
    identifier issn0739-0572
    identifier otherams-69276.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210927
    description abstractA method is proposed to retrieve raindrop shape?size relations from the radar measurements of reflectivity factor Zh, differential reflectivity Zdr, and specific differential phase Kdp at S band. This procedure is obtained using a domain defined by the two variables Kdp/Zh and Zdr where the drop size distribution (DSD) variability is collapsed onto a line and any variation is essentially due to the drop shape variability. To obtain information on the raindrop shape?size relation underlying a set of radar observations, this domain is studied in conjunction with another domain describing the relation between the drop axial ratio (or shape) and its equivolumetric diameter. Using an initial drop shape and choosing a set of DSDs described by a normalized gamma model, polarimetric radar measurements are produced by simulation. An averaged curve of Kdp/Zh versus Zdr is obtained and compared with the same curve obtained from the radar data. By changing the initial axial ratio relation, a procedure of minimization between the two curves is developed to derive the underlying drop shape?size relation governing the radar measurements under consideration. Three sets of radar data collected in different climatic regions are analyzed to evaluate whether there is a unique shape?size relation.
    publisherAmerican Meteorological Society
    titleCan a Unique Model Describe the Raindrop Shape–Size Relation? A Clue from Polarimetric Radar Measurements
    typeJournal Paper
    journal volume26
    journal issue9
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/2009JTECHA1183.1
    journal fristpage1829
    journal lastpage1842
    treeJournal of Atmospheric and Oceanic Technology:;2009:;volume( 026 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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