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    A Study of Lateral and Longitudinal Intensities of Turbulence

    Source: Journal of Applied Meteorology:;1965:;volume( 004 ):;issue: 003::page 409
    Author:
    Swanson, R. N.
    ,
    Cramer, H. E.
    DOI: 10.1175/1520-0450(1965)004<0409:ASOLAL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An analysis of the lateral and longitudinal intensifies of turbulence measured on a 62-m meteorological tower over a two-year period at White Sands Missile Range shows that both intensifies decrease with height in all thermal stratifications. This decrease can be expressed in terms of a simple power law in which the value of the exponent on height varies from about ?0.1 to ?0.3 as the stratification changes from lapse to inversion. Also, the turbulent intensifies at all heights and in all thermal stratification tend to be inversely proportional to the mean wind speed. This relationship is most pronounced during lapse conditions when the product of mean wind speed and turbulent intensity is practically constant. Diurnal variations of the intensifies at five heights are presented for three wind speed regimes, and the results are compared with measurements made previously at other locations.
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      A Study of Lateral and Longitudinal Intensities of Turbulence

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4214223
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    contributor authorSwanson, R. N.
    contributor authorCramer, H. E.
    date accessioned2017-06-09T16:41:17Z
    date available2017-06-09T16:41:17Z
    date copyright1965/06/01
    date issued1965
    identifier issn0021-8952
    identifier otherams-7224.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214223
    description abstractAn analysis of the lateral and longitudinal intensifies of turbulence measured on a 62-m meteorological tower over a two-year period at White Sands Missile Range shows that both intensifies decrease with height in all thermal stratifications. This decrease can be expressed in terms of a simple power law in which the value of the exponent on height varies from about ?0.1 to ?0.3 as the stratification changes from lapse to inversion. Also, the turbulent intensifies at all heights and in all thermal stratification tend to be inversely proportional to the mean wind speed. This relationship is most pronounced during lapse conditions when the product of mean wind speed and turbulent intensity is practically constant. Diurnal variations of the intensifies at five heights are presented for three wind speed regimes, and the results are compared with measurements made previously at other locations.
    publisherAmerican Meteorological Society
    titleA Study of Lateral and Longitudinal Intensities of Turbulence
    typeJournal Paper
    journal volume4
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1965)004<0409:ASOLAL>2.0.CO;2
    journal fristpage409
    journal lastpage417
    treeJournal of Applied Meteorology:;1965:;volume( 004 ):;issue: 003
    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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