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    POWER SPECTRA OF THE EDDY-VELOCITY COMPONENTS

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 002::page 146
    Author:
    Cramer, Harrison E.
    ,
    Record, Frank A.
    DOI: 10.1175/1520-0469(1955)012<0146:PSOTEV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Power spectra of the eddy-velocity components have been determined at four levels within the layer from 2 to 12 meters under varying conditions of mean wind speed, trajectory and thermal stability. A filtering technique suggested by J. W. Tukey has been used to obtain rough estimates of contributions to the total variance for seven consecutive frequency intervals within the range from about 0.5 to 0.005 cycles per second. At the higher frequencies studied, variances for all three components are approximately equal and equipartition of turbulent energy is thus indicated. Spectra for the u- and v-components appear to be invariant with frequency at the lowest level, and tend to increase slowly with decreasing frequency at the higher levels. The w-spectra at all levels fall off sharply with decreasing frequency, contributions to the vertically-directed energy becoming almost negligible at the lowest frequencies investigated.
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      POWER SPECTRA OF THE EDDY-VELOCITY COMPONENTS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149681
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    contributor authorCramer, Harrison E.
    contributor authorRecord, Frank A.
    date accessioned2017-06-09T14:11:12Z
    date available2017-06-09T14:11:12Z
    date copyright1955/04/01
    date issued1955
    identifier issn0095-9634
    identifier otherams-14151.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149681
    description abstractPower spectra of the eddy-velocity components have been determined at four levels within the layer from 2 to 12 meters under varying conditions of mean wind speed, trajectory and thermal stability. A filtering technique suggested by J. W. Tukey has been used to obtain rough estimates of contributions to the total variance for seven consecutive frequency intervals within the range from about 0.5 to 0.005 cycles per second. At the higher frequencies studied, variances for all three components are approximately equal and equipartition of turbulent energy is thus indicated. Spectra for the u- and v-components appear to be invariant with frequency at the lowest level, and tend to increase slowly with decreasing frequency at the higher levels. The w-spectra at all levels fall off sharply with decreasing frequency, contributions to the vertically-directed energy becoming almost negligible at the lowest frequencies investigated.
    publisherAmerican Meteorological Society
    titlePOWER SPECTRA OF THE EDDY-VELOCITY COMPONENTS
    typeJournal Paper
    journal volume12
    journal issue2
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1955)012<0146:PSOTEV>2.0.CO;2
    journal fristpage146
    journal lastpage151
    treeJournal of Meteorology:;1955:;volume( 012 ):;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
    yabeshDSpacePersian