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    Cirrus Cloud Microphysical Property Retrieval Using Lidar and Radar Measurements. Part I: Algorithm Description and Comparison with In Situ Data

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 003::page 218
    Author:
    Wang, Zhien
    ,
    Sassen, Kenneth
    DOI: 10.1175/1520-0450(2002)041<0218:CCMPRU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A retrieval algorithm is described to estimate vertical profiles of cirrus-cloud ice water content (IWC) and general effective size Dge from combined lidar and radar measurements. In the algorithm, the lidar extinction coefficient σ is parameterized as σ = IWC[a0 + (a1/Dge)] and water equivalent radar reflectivity factor Ze is parameterized as Ze = C?(IWC/?i)Dbge, where a0, a1, C?, and b are constants based on the assumption of a modified gamma size distribution and hexagonal ice crystals. A comparison of retrieved results from a cirrus-cloud case study with aircraft in situ measurements indicates that the algorithm can provide reliable cirrus cloud microphysical properties. A technique to estimate ice water path and layer-mean Dge is also developed using the optical depth and mean radar reflectivity factor of the cloud layer.
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      Cirrus Cloud Microphysical Property Retrieval Using Lidar and Radar Measurements. Part I: Algorithm Description and Comparison with In Situ Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148538
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    contributor authorWang, Zhien
    contributor authorSassen, Kenneth
    date accessioned2017-06-09T14:08:20Z
    date available2017-06-09T14:08:20Z
    date copyright2002/03/01
    date issued2002
    identifier issn0894-8763
    identifier otherams-13122.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148538
    description abstractA retrieval algorithm is described to estimate vertical profiles of cirrus-cloud ice water content (IWC) and general effective size Dge from combined lidar and radar measurements. In the algorithm, the lidar extinction coefficient σ is parameterized as σ = IWC[a0 + (a1/Dge)] and water equivalent radar reflectivity factor Ze is parameterized as Ze = C?(IWC/?i)Dbge, where a0, a1, C?, and b are constants based on the assumption of a modified gamma size distribution and hexagonal ice crystals. A comparison of retrieved results from a cirrus-cloud case study with aircraft in situ measurements indicates that the algorithm can provide reliable cirrus cloud microphysical properties. A technique to estimate ice water path and layer-mean Dge is also developed using the optical depth and mean radar reflectivity factor of the cloud layer.
    publisherAmerican Meteorological Society
    titleCirrus Cloud Microphysical Property Retrieval Using Lidar and Radar Measurements. Part I: Algorithm Description and Comparison with In Situ Data
    typeJournal Paper
    journal volume41
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2002)041<0218:CCMPRU>2.0.CO;2
    journal fristpage218
    journal lastpage229
    treeJournal of Applied Meteorology:;2002:;volume( 041 ):;issue: 003
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian