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    Horizontal Dispersion Parameters for Long-Range Transport Modeling

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 003::page 367
    Author:
    Draxler, Roland R.
    ,
    Taylor, Albion D.
    DOI: 10.1175/1520-0450(1982)021<0367:HDPFLR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A computer model using actual meteorological data is developed to simulate the effects of wind shear on an instantaneous pollutant puff. The effect of wind shear on dispersion is obtained by subdividing, during the nocturnal phase, the previous daytime pollutant mixed layer into 300 m layers. Each layer is tracked as a separate trajectory. Vertical mixing is resumed during the next daytime phase. Further subdivisions occur each nocturnal phase. The computer simulation of puff growth as a result of shear confirmed the proportionality of puff spread to geostrophic wind speed during homogeneous conditions as derived by Taylor (1982). Both Taylor's and the computer simulation results are consistent with published experimental long-range dispersion data representative of average conditions.
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      Horizontal Dispersion Parameters for Long-Range Transport Modeling

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145321
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    contributor authorDraxler, Roland R.
    contributor authorTaylor, Albion D.
    date accessioned2017-06-09T13:58:39Z
    date available2017-06-09T13:58:39Z
    date copyright1982/03/01
    date issued1982
    identifier issn0021-8952
    identifier otherams-10227.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145321
    description abstractA computer model using actual meteorological data is developed to simulate the effects of wind shear on an instantaneous pollutant puff. The effect of wind shear on dispersion is obtained by subdividing, during the nocturnal phase, the previous daytime pollutant mixed layer into 300 m layers. Each layer is tracked as a separate trajectory. Vertical mixing is resumed during the next daytime phase. Further subdivisions occur each nocturnal phase. The computer simulation of puff growth as a result of shear confirmed the proportionality of puff spread to geostrophic wind speed during homogeneous conditions as derived by Taylor (1982). Both Taylor's and the computer simulation results are consistent with published experimental long-range dispersion data representative of average conditions.
    publisherAmerican Meteorological Society
    titleHorizontal Dispersion Parameters for Long-Range Transport Modeling
    typeJournal Paper
    journal volume21
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1982)021<0367:HDPFLR>2.0.CO;2
    journal fristpage367
    journal lastpage372
    treeJournal of Applied Meteorology:;1982:;volume( 021 ):;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
    yabeshDSpacePersian