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    INSTANTANEOUS AND CONTINUOUS WIND MEASUREMENTS UP TO THE HIGHER STRATOSPHERE

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 005::page 448
    Author:
    Reisig, Gerhard H. R.
    DOI: 10.1175/1520-0469(1956)013<0448:IACWMU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A method is presented of measuring the wind velocity as actually encountered during a guided missile flight. This wind measurement is instantaneous and continuous. The measuring quantities involved are the velocity vector of the missile relative to the ground (obtained by flight-path tracking), the missile-axis attitude angles (provided by on-board gyros), and the angle of attack (measured by an airflow-direction meter at the missile nose). The basic assumption for the wind determination is an always horizontal wind vector. The method yields wind information to an altitude of 60 kilometers with the presently available instrumentation. The measuring time to this altitude is less than 2½ minutes. Three wind profiles measured at different seasons of the year are presented, with relevant rawinsonde measurements for comparison. Also, the instantaneous vertical wind gradients are derived; they represent true physical quantities, because they are obtained from continuous wind-velocity measurements without averaging.
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      INSTANTANEOUS AND CONTINUOUS WIND MEASUREMENTS UP TO THE HIGHER STRATOSPHERE

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4149841
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    contributor authorReisig, Gerhard H. R.
    date accessioned2017-06-09T14:11:32Z
    date available2017-06-09T14:11:32Z
    date copyright1956/10/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14296.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149841
    description abstractA method is presented of measuring the wind velocity as actually encountered during a guided missile flight. This wind measurement is instantaneous and continuous. The measuring quantities involved are the velocity vector of the missile relative to the ground (obtained by flight-path tracking), the missile-axis attitude angles (provided by on-board gyros), and the angle of attack (measured by an airflow-direction meter at the missile nose). The basic assumption for the wind determination is an always horizontal wind vector. The method yields wind information to an altitude of 60 kilometers with the presently available instrumentation. The measuring time to this altitude is less than 2½ minutes. Three wind profiles measured at different seasons of the year are presented, with relevant rawinsonde measurements for comparison. Also, the instantaneous vertical wind gradients are derived; they represent true physical quantities, because they are obtained from continuous wind-velocity measurements without averaging.
    publisherAmerican Meteorological Society
    titleINSTANTANEOUS AND CONTINUOUS WIND MEASUREMENTS UP TO THE HIGHER STRATOSPHERE
    typeJournal Paper
    journal volume13
    journal issue5
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0448:IACWMU>2.0.CO;2
    journal fristpage448
    journal lastpage456
    treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 005
    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