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    An Airborne Laser Air Motion Sensing System. Part II: Design Criteria and Measurement Possibilities

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 001::page 128
    Author:
    Kristensen, Leif
    ,
    Lenschow, Donald H.
    DOI: 10.1175/1520-0426(1987)004<0128:AALAMS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A conically scanning Doppler lidar technique for measuring air motions from an aircraft is proposed in the companion paper (Keeler et al.). A theoretical analysis of this technique shows that, assuming isotropic turbulence, the technique is feasible for measuring air motions to woes small enough that the velocity spectra in a convective atmospheric boundary layer can be resolved well into the inertial subrange, and most of the turbulent motions that contribute to the vertical fluxes can be resolved. A scanning beam range of 10 m was selected to ensure that flow distortion induced by the aircraft will not significantly affect the velocity measurement. Thus, the technique offers improved accuracy over presently used immersion air motion sensors. An additional feature is the possibility of measuring mean vertical wind shear.
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      An Airborne Laser Air Motion Sensing System. Part II: Design Criteria and Measurement Possibilities

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4164178
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    contributor authorKristensen, Leif
    contributor authorLenschow, Donald H.
    date accessioned2017-06-09T14:48:26Z
    date available2017-06-09T14:48:26Z
    date copyright1987/03/01
    date issued1987
    identifier issn0739-0572
    identifier otherams-272.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164178
    description abstractA conically scanning Doppler lidar technique for measuring air motions from an aircraft is proposed in the companion paper (Keeler et al.). A theoretical analysis of this technique shows that, assuming isotropic turbulence, the technique is feasible for measuring air motions to woes small enough that the velocity spectra in a convective atmospheric boundary layer can be resolved well into the inertial subrange, and most of the turbulent motions that contribute to the vertical fluxes can be resolved. A scanning beam range of 10 m was selected to ensure that flow distortion induced by the aircraft will not significantly affect the velocity measurement. Thus, the technique offers improved accuracy over presently used immersion air motion sensors. An additional feature is the possibility of measuring mean vertical wind shear.
    publisherAmerican Meteorological Society
    titleAn Airborne Laser Air Motion Sensing System. Part II: Design Criteria and Measurement Possibilities
    typeJournal Paper
    journal volume4
    journal issue1
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1987)004<0128:AALAMS>2.0.CO;2
    journal fristpage128
    journal lastpage138
    treeJournal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;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
    yabeshDSpacePersian