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    Averaging for Wind Speed in a Given Direction in the Concentration Equation for Pollutants

    Source: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 010::page 1097
    Author:
    Neumann, J.
    DOI: 10.1175/1520-0450-16.10.1097
    Publisher: American Meteorological Society
    Abstract: In the equation for the concentration of pollutants from a steady continuous point source, in a stationaryturbulent flow, the factor 1/u enters (u is the mean wind for a given stationary situation). If we are interestedin the concentration along a given wind direction and u denotes the wind speed in that direction and if weseek the average concentration for a class of flow situations (e.g., for the class of statically stable flows),each member of the class representing an individual stationary situation, then the averaging to be appliedis to 1/u and not to u. On the assumption (verified by some examples) that the distribution of u isa "humped" gamma distribution (standard deviation σ less than the average u of u for the class as a whole),we show that the average of 1/u equals 1/(u[1-(σ/u)2]}. Thus the average of 1/u is greater than 1/uand the resulting concentration estimate is larger than the one that would be obtained by the incorrect useof 1/u.
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      Averaging for Wind Speed in a Given Direction in the Concentration Equation for Pollutants

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4148869
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    contributor authorNeumann, J.
    date accessioned2017-06-09T14:09:19Z
    date available2017-06-09T14:09:19Z
    date copyright1977/10/01
    date issued1977
    identifier issn0021-8952
    identifier otherams-13420.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148869
    description abstractIn the equation for the concentration of pollutants from a steady continuous point source, in a stationaryturbulent flow, the factor 1/u enters (u is the mean wind for a given stationary situation). If we are interestedin the concentration along a given wind direction and u denotes the wind speed in that direction and if weseek the average concentration for a class of flow situations (e.g., for the class of statically stable flows),each member of the class representing an individual stationary situation, then the averaging to be appliedis to 1/u and not to u. On the assumption (verified by some examples) that the distribution of u isa "humped" gamma distribution (standard deviation σ less than the average u of u for the class as a whole),we show that the average of 1/u equals 1/(u[1-(σ/u)2]}. Thus the average of 1/u is greater than 1/uand the resulting concentration estimate is larger than the one that would be obtained by the incorrect useof 1/u.
    publisherAmerican Meteorological Society
    titleAveraging for Wind Speed in a Given Direction in the Concentration Equation for Pollutants
    typeJournal Paper
    journal volume16
    journal issue10
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450-16.10.1097
    journal fristpage1097
    journal lastpage1100
    treeJournal of Applied Meteorology:;1977:;volume( 016 ):;issue: 010
    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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