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    The Convective Boundary Layer Structure from Lidar and Radiosonde Measurements during the EFEDA '91 Campaign

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 004::page 771
    Author:
    Kiemle, C.
    ,
    Kästner, M.
    ,
    Ehret, C.
    DOI: 10.1175/1520-0426(1995)012<0771:TCBLSF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The convective boundary layer has been investigated with an airborne differential absorption lidar (DIAL) during the EFEDA (European Field Experiment in a Desertification Threatened Area) campaign in June 1991 over middle Spain. For the first time, airborne DIAL water vapor measurements resolving the structure of a convection cell are presented. On 28 June, an interesting boundary layer structure has been found in the lidar aerosol and water vapor measurements, showing a wave structure with a wavelength of 4.5 km and an amplitude of 100?450 m in the residual layer. Additional radiosonde data and the analysis of the synoptic situation reveal that this wave structure is part of a wind shear-driven gravity wave.
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      The Convective Boundary Layer Structure from Lidar and Radiosonde Measurements during the EFEDA '91 Campaign

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145823
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    contributor authorKiemle, C.
    contributor authorKästner, M.
    contributor authorEhret, C.
    date accessioned2017-06-09T14:00:04Z
    date available2017-06-09T14:00:04Z
    date copyright1995/08/01
    date issued1995
    identifier issn0739-0572
    identifier otherams-1068.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145823
    description abstractThe convective boundary layer has been investigated with an airborne differential absorption lidar (DIAL) during the EFEDA (European Field Experiment in a Desertification Threatened Area) campaign in June 1991 over middle Spain. For the first time, airborne DIAL water vapor measurements resolving the structure of a convection cell are presented. On 28 June, an interesting boundary layer structure has been found in the lidar aerosol and water vapor measurements, showing a wave structure with a wavelength of 4.5 km and an amplitude of 100?450 m in the residual layer. Additional radiosonde data and the analysis of the synoptic situation reveal that this wave structure is part of a wind shear-driven gravity wave.
    publisherAmerican Meteorological Society
    titleThe Convective Boundary Layer Structure from Lidar and Radiosonde Measurements during the EFEDA '91 Campaign
    typeJournal Paper
    journal volume12
    journal issue4
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1995)012<0771:TCBLSF>2.0.CO;2
    journal fristpage771
    journal lastpage782
    treeJournal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 004
    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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