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    APPLICATION OF THE STATISTICAL THEORY OF TURBULENT DIFFUSION TO MICROMETEOROLOGY

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 004::page 252
    Author:
    Frenkiel, F. N.
    DOI: 10.1175/1520-0469(1952)009<0252:AOTSTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Some elements of the statistical theory of turbulence are briefly reviewed from the viewpoint of their application to micrometeorology.Several relations concerning turbulent diffusion in a field of homogeneous and isotropic turbulence are then discussed. The mean-concentration distributions for an instantaneous and for a continuous point-source are investigated, with particular attention to the case when the intensity of turbulence cannot be considered as small in comparison with the mean velocity. The time history of mean-concentration distributions in a diffusing spherical cloud is then studied. The relation between Fick's differential equation of diffusion and the statistical theory of turbulence is studied, and the limits of validity of Fick's equation are determined. Finally, the relation between the coefficient of eddy diffusion and the statistical characteristics of turbulence is discussed.
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      APPLICATION OF THE STATISTICAL THEORY OF TURBULENT DIFFUSION TO MICROMETEOROLOGY

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4149421
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    contributor authorFrenkiel, F. N.
    date accessioned2017-06-09T14:10:35Z
    date available2017-06-09T14:10:35Z
    date copyright1952/08/01
    date issued1952
    identifier issn0095-9634
    identifier otherams-13918.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149421
    description abstractSome elements of the statistical theory of turbulence are briefly reviewed from the viewpoint of their application to micrometeorology.Several relations concerning turbulent diffusion in a field of homogeneous and isotropic turbulence are then discussed. The mean-concentration distributions for an instantaneous and for a continuous point-source are investigated, with particular attention to the case when the intensity of turbulence cannot be considered as small in comparison with the mean velocity. The time history of mean-concentration distributions in a diffusing spherical cloud is then studied. The relation between Fick's differential equation of diffusion and the statistical theory of turbulence is studied, and the limits of validity of Fick's equation are determined. Finally, the relation between the coefficient of eddy diffusion and the statistical characteristics of turbulence is discussed.
    publisherAmerican Meteorological Society
    titleAPPLICATION OF THE STATISTICAL THEORY OF TURBULENT DIFFUSION TO MICROMETEOROLOGY
    typeJournal Paper
    journal volume9
    journal issue4
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1952)009<0252:AOTSTO>2.0.CO;2
    journal fristpage252
    journal lastpage259
    treeJournal of Meteorology:;1952:;volume( 009 ):;issue: 004
    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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