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    Measurement of Water Vapor Flux Profiles in the Convective Boundary Layer with Lidar and Radar-RASS

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 001::page 85
    Author:
    Senff, Christoph
    ,
    Bösenberg, Jens
    ,
    Peters, Gerhard
    DOI: 10.1175/1520-0426(1994)011<0085:MOWVFP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A remote-sensing method to retrieve vertical profiles of water vapor flux in the convective boundary layer by using a differential absorption lidar and a radar-radio acoustic sounding system is described. The system's height range presently extends from 400 to 700 m above the surface, and flux data can be sampled with a height resolution of 75 m and a time resolution of 60 s. The results of a first measurement in July 1991 under predominantly convective conditions are presented. The resolution of the remote-sensing system apparently is sufficient to resolve the major contributions to the flux in the convective mixed layer. In addition, the advantages and limitations of this method are discussed.
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      Measurement of Water Vapor Flux Profiles in the Convective Boundary Layer with Lidar and Radar-RASS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4230844
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorSenff, Christoph
    contributor authorBösenberg, Jens
    contributor authorPeters, Gerhard
    date accessioned2017-06-09T17:33:34Z
    date available2017-06-09T17:33:34Z
    date copyright1994/02/01
    date issued1994
    identifier issn0739-0572
    identifier otherams-872.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230844
    description abstractA remote-sensing method to retrieve vertical profiles of water vapor flux in the convective boundary layer by using a differential absorption lidar and a radar-radio acoustic sounding system is described. The system's height range presently extends from 400 to 700 m above the surface, and flux data can be sampled with a height resolution of 75 m and a time resolution of 60 s. The results of a first measurement in July 1991 under predominantly convective conditions are presented. The resolution of the remote-sensing system apparently is sufficient to resolve the major contributions to the flux in the convective mixed layer. In addition, the advantages and limitations of this method are discussed.
    publisherAmerican Meteorological Society
    titleMeasurement of Water Vapor Flux Profiles in the Convective Boundary Layer with Lidar and Radar-RASS
    typeJournal Paper
    journal volume11
    journal issue1
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1994)011<0085:MOWVFP>2.0.CO;2
    journal fristpage85
    journal lastpage93
    treeJournal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 001
    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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