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    Acoustic Component of Turbulence

    Source: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 002::page 286
    Author:
    Webb, Willis L.
    DOI: 10.1175/1520-0450(1963)002<0286:ACOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The intimate relationship between the local speed of sound of a flight environment and the lift and/or drag on a vehicle is discussed. The fact that this parameter will become increasingly significant as the speed increases is pointed out. In addition, it is noted that the usual source of flight ?bumpiness? (i.e., wind variations) tends to become less effective as the speed increases. Examples of the sonic gradients which have thus far been observed in the high altitude regions of the earth's atmosphere are presented, and the circumstances under which such gradients would be most elective in perturbing a particular flight path are described. It is concluded that the variable vehicle loads imposed by atmospheric structure are composed of flow and thermo-dynamic components, and that both of these atmospheric parameters must be studied in the light of our expanding speeds and spatial activities.
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      Acoustic Component of Turbulence

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211233
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    contributor authorWebb, Willis L.
    date accessioned2017-06-09T16:32:04Z
    date available2017-06-09T16:32:04Z
    date copyright1963/04/01
    date issued1963
    identifier issn0021-8952
    identifier otherams-6955.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211233
    description abstractThe intimate relationship between the local speed of sound of a flight environment and the lift and/or drag on a vehicle is discussed. The fact that this parameter will become increasingly significant as the speed increases is pointed out. In addition, it is noted that the usual source of flight ?bumpiness? (i.e., wind variations) tends to become less effective as the speed increases. Examples of the sonic gradients which have thus far been observed in the high altitude regions of the earth's atmosphere are presented, and the circumstances under which such gradients would be most elective in perturbing a particular flight path are described. It is concluded that the variable vehicle loads imposed by atmospheric structure are composed of flow and thermo-dynamic components, and that both of these atmospheric parameters must be studied in the light of our expanding speeds and spatial activities.
    publisherAmerican Meteorological Society
    titleAcoustic Component of Turbulence
    typeJournal Paper
    journal volume2
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1963)002<0286:ACOT>2.0.CO;2
    journal fristpage286
    journal lastpage291
    treeJournal of Applied Meteorology:;1963:;volume( 002 ):;issue: 002
    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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