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    A Method for Determining Cirrus Cloud Particle Sizes Using Lidar and Radar Backscatter Technique

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 006::page 1074
    Author:
    Intrieri, Janet M.
    ,
    Stephens, Graeme L.
    ,
    Eberhard, Wynn L.
    ,
    Uttal, Taneil
    DOI: 10.1175/1520-0450(1993)032<1074:AMFDCC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A method to determine cirrus cloud effective radii remotely using lidar and radar backscatter data is presented. The difference in backscattered returns from instruments widely separated in wavelength holds information on the characteristic sizes of the scatterers. The method compares theoretically expected backscatter coefficients to observed backscatter returns from NOAA's 3.2-cm and 8.6-mm radars and the 10.6-µm lidar. Measurements were taken during a two-phase cloud experiment held in northeastern Colorado from 6 September to 5 October 1989 and 15 February to 31 March 1991. It was found that the particle sizes estimated from the lidar-radar method agree closely with in situ aircraft measurements. Case studies are presented to demonstrate the method and the potential for multiwavelength remote sensing of cirrus cloud radiative properties.
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      A Method for Determining Cirrus Cloud Particle Sizes Using Lidar and Radar Backscatter Technique

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4147207
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    • Journal of Applied Meteorology

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    contributor authorIntrieri, Janet M.
    contributor authorStephens, Graeme L.
    contributor authorEberhard, Wynn L.
    contributor authorUttal, Taneil
    date accessioned2017-06-09T14:04:27Z
    date available2017-06-09T14:04:27Z
    date copyright1993/06/01
    date issued1993
    identifier issn0894-8763
    identifier otherams-11925.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147207
    description abstractA method to determine cirrus cloud effective radii remotely using lidar and radar backscatter data is presented. The difference in backscattered returns from instruments widely separated in wavelength holds information on the characteristic sizes of the scatterers. The method compares theoretically expected backscatter coefficients to observed backscatter returns from NOAA's 3.2-cm and 8.6-mm radars and the 10.6-µm lidar. Measurements were taken during a two-phase cloud experiment held in northeastern Colorado from 6 September to 5 October 1989 and 15 February to 31 March 1991. It was found that the particle sizes estimated from the lidar-radar method agree closely with in situ aircraft measurements. Case studies are presented to demonstrate the method and the potential for multiwavelength remote sensing of cirrus cloud radiative properties.
    publisherAmerican Meteorological Society
    titleA Method for Determining Cirrus Cloud Particle Sizes Using Lidar and Radar Backscatter Technique
    typeJournal Paper
    journal volume32
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1993)032<1074:AMFDCC>2.0.CO;2
    journal fristpage1074
    journal lastpage1082
    treeJournal of Applied Meteorology:;1993:;volume( 032 ):;issue: 006
    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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