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    Diffusion of Clouds of Contaminant in a Turbulent Boundary Layer

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 004::page 387
    Author:
    O'Brien, Edward E.
    DOI: 10.1175/1520-0469(1966)023<0387:DOCOCI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Under the assumption that the detailed turbulence structure in the constant-stress region of a fluid flowing over a rough wall is in a universal state determined wholly by the friction velocity u* a similarity analysis of a Lagrangian type can be applied to the relative dispersion of clouds of contaminant released in such a layer. It is found that for the case in which the initial dimension of the cloud, say L, and the initial mean height are comparable, there are only two temporal regimes and they are characterized by times smaller than or greater than L/u*. For the small time regime all relative diffusivities are linearly dependent on time and their directional properties are related to Eulerian measurements. Of more interest are the predictions in the long time regime. It is also found in this region that relative diffusion is characterized by a diffusivity that is linearly dependent on time. Such a prediction differs from that of homogeneous turbulence and seems to have some support from experimental data in the earth's atmosphere.
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      Diffusion of Clouds of Contaminant in a Turbulent Boundary Layer

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    contributor authorO'Brien, Edward E.
    date accessioned2017-06-09T14:13:50Z
    date available2017-06-09T14:13:50Z
    date copyright1966/07/01
    date issued1966
    identifier issn0022-4928
    identifier otherams-15211.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150859
    description abstractUnder the assumption that the detailed turbulence structure in the constant-stress region of a fluid flowing over a rough wall is in a universal state determined wholly by the friction velocity u* a similarity analysis of a Lagrangian type can be applied to the relative dispersion of clouds of contaminant released in such a layer. It is found that for the case in which the initial dimension of the cloud, say L, and the initial mean height are comparable, there are only two temporal regimes and they are characterized by times smaller than or greater than L/u*. For the small time regime all relative diffusivities are linearly dependent on time and their directional properties are related to Eulerian measurements. Of more interest are the predictions in the long time regime. It is also found in this region that relative diffusion is characterized by a diffusivity that is linearly dependent on time. Such a prediction differs from that of homogeneous turbulence and seems to have some support from experimental data in the earth's atmosphere.
    publisherAmerican Meteorological Society
    titleDiffusion of Clouds of Contaminant in a Turbulent Boundary Layer
    typeJournal Paper
    journal volume23
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1966)023<0387:DOCOCI>2.0.CO;2
    journal fristpage387
    journal lastpage389
    treeJournal of the Atmospheric Sciences:;1966:;Volume( 023 ):;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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