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    Analog Computing Techniques Applied to Atmospheric Diffusion: Continuous Point Source

    Source: Journal of Applied Meteorology:;1963:;volume( 002 ):;issue: 001::page 129
    Author:
    Brock, Fred V.
    ,
    Hewson, E. Wendell
    DOI: 10.1175/1520-0450(1963)002<0129:ACTATA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The analog computer has been used to obtain solutions to the diffusion equation for the case of a continuous point source aloft. The basic model used is that of a source located between an inversion and the ground where the wind speed and eddy diffusivity are constant over the diffusing region. Solutions were also obtained with several special features added to the basic model: representation of the eddy diffusivity as a function of distance downstream; presence of wind direction shear in the diffusing layers; and the presence of large-scale eddies which cause the meandering of the plume. The solutions are presented as deviations from the reference solution, that solution derived from the basic model, to show graphically the effects of each parameter change.
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      Analog Computing Techniques Applied to Atmospheric Diffusion: Continuous Point Source

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4210978
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    • Journal of Applied Meteorology

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    contributor authorBrock, Fred V.
    contributor authorHewson, E. Wendell
    date accessioned2017-06-09T16:31:15Z
    date available2017-06-09T16:31:15Z
    date copyright1963/02/01
    date issued1963
    identifier issn0021-8952
    identifier otherams-6932.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210978
    description abstractThe analog computer has been used to obtain solutions to the diffusion equation for the case of a continuous point source aloft. The basic model used is that of a source located between an inversion and the ground where the wind speed and eddy diffusivity are constant over the diffusing region. Solutions were also obtained with several special features added to the basic model: representation of the eddy diffusivity as a function of distance downstream; presence of wind direction shear in the diffusing layers; and the presence of large-scale eddies which cause the meandering of the plume. The solutions are presented as deviations from the reference solution, that solution derived from the basic model, to show graphically the effects of each parameter change.
    publisherAmerican Meteorological Society
    titleAnalog Computing Techniques Applied to Atmospheric Diffusion: Continuous Point Source
    typeJournal Paper
    journal volume2
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1963)002<0129:ACTATA>2.0.CO;2
    journal fristpage129
    journal lastpage144
    treeJournal of Applied Meteorology:;1963:;volume( 002 ):;issue: 001
    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