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    A Hydrometeor Classification Method for X-Band Polarimetric Radar: Construction and Validation Focusing on Solid Hydrometeors under Moist Environments

    Source: Journal of Atmospheric and Oceanic Technology:;2015:;volume( 032 ):;issue: 011::page 2052
    Author:
    Kouketsu, Takeharu
    ,
    Uyeda, Hiroshi
    ,
    Ohigashi, Tadayasu
    ,
    Oue, Mariko
    ,
    Takeuchi, Hiroto
    ,
    Shinoda, Taro
    ,
    Tsuboki, Kazuhisa
    ,
    Kubo, Mamoru
    ,
    Muramoto, Ken-ichiro
    DOI: 10.1175/JTECH-D-14-00124.1
    Publisher: American Meteorological Society
    Abstract: fuzzy-logic-based hydrometeor classification (HC) method for X-band polarimetric radar (X-pol), which is suitable for observation of solid hydrometeors under moist environments producing little or no hail, is constructed and validated. This HC method identifies the most likely hydrometeor at each radar sampling volume from eight categories: 1) drizzle, 2) rain, 3) wet snow aggregates, 4) dry snow aggregates, 5) ice crystals, 6) dry graupel, 7) wet graupel, and 8) rain?hail mixture. Membership functions are defined on the basis of previous studies. The HC method uses radar reflectivity Zh, differential reflectivity Zdr, specific differential phase Kdp, and correlation coefficient ?hv as its main inputs, and temperature with some consideration of relative humidity as supplemental information. The method is validated against ground and in situ observations of solid hydrometeors (dry graupel, dry snow aggregates, and ice crystals) under a moist environment. Observational data from a ground-based imaging system are used to validate the HC method for dry graupel and dry snow aggregates. For dry snow aggregates and ice crystals, the HC method is validated using simultaneous observations from a balloonborne instrument [hydrometeor videosonde (HYVIS)] and an X-pol range?height indicator directed toward the HYVIS. The HC method distinguishes effectively between dry graupel, dry snow aggregates, and ice crystals, and is therefore valid for HC under moist environments.
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      A Hydrometeor Classification Method for X-Band Polarimetric Radar: Construction and Validation Focusing on Solid Hydrometeors under Moist Environments

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228561
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorKouketsu, Takeharu
    contributor authorUyeda, Hiroshi
    contributor authorOhigashi, Tadayasu
    contributor authorOue, Mariko
    contributor authorTakeuchi, Hiroto
    contributor authorShinoda, Taro
    contributor authorTsuboki, Kazuhisa
    contributor authorKubo, Mamoru
    contributor authorMuramoto, Ken-ichiro
    date accessioned2017-06-09T17:25:57Z
    date available2017-06-09T17:25:57Z
    date copyright2015/11/01
    date issued2015
    identifier issn0739-0572
    identifier otherams-85146.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228561
    description abstractfuzzy-logic-based hydrometeor classification (HC) method for X-band polarimetric radar (X-pol), which is suitable for observation of solid hydrometeors under moist environments producing little or no hail, is constructed and validated. This HC method identifies the most likely hydrometeor at each radar sampling volume from eight categories: 1) drizzle, 2) rain, 3) wet snow aggregates, 4) dry snow aggregates, 5) ice crystals, 6) dry graupel, 7) wet graupel, and 8) rain?hail mixture. Membership functions are defined on the basis of previous studies. The HC method uses radar reflectivity Zh, differential reflectivity Zdr, specific differential phase Kdp, and correlation coefficient ?hv as its main inputs, and temperature with some consideration of relative humidity as supplemental information. The method is validated against ground and in situ observations of solid hydrometeors (dry graupel, dry snow aggregates, and ice crystals) under a moist environment. Observational data from a ground-based imaging system are used to validate the HC method for dry graupel and dry snow aggregates. For dry snow aggregates and ice crystals, the HC method is validated using simultaneous observations from a balloonborne instrument [hydrometeor videosonde (HYVIS)] and an X-pol range?height indicator directed toward the HYVIS. The HC method distinguishes effectively between dry graupel, dry snow aggregates, and ice crystals, and is therefore valid for HC under moist environments.
    publisherAmerican Meteorological Society
    titleA Hydrometeor Classification Method for X-Band Polarimetric Radar: Construction and Validation Focusing on Solid Hydrometeors under Moist Environments
    typeJournal Paper
    journal volume32
    journal issue11
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/JTECH-D-14-00124.1
    journal fristpage2052
    journal lastpage2074
    treeJournal of Atmospheric and Oceanic Technology:;2015:;volume( 032 ):;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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