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    A PRELIMINARY EVALUATION OF SUTTON'S HYPOTHESIS FOR DIFFUSION FROM A CONTINUOUS POINT SOURCE

    Source: Journal of Meteorology:;1959:;volume( 016 ):;issue: 001::page 12
    Author:
    Barad, Morton L.
    ,
    Haugen, Duane A.
    DOI: 10.1175/1520-0469(1959)016<0012:APEOSH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Sutton's hypothesis for diffusion from a continuous point source has been evaluated using the data obtained during Project Prairie Grass. It is found that the hypothesis predicts the observed concentration distributions only if there are two values of Sutton's ?n?, one to characterize lateral diffusion (ny) and one to characterize vertical diffusion (nz). Statistical tests indicate that ny and nz are invariant with distance between 100 and 800 m of the source, but that the values of ny and nz appropriate for these distances exceed the values within 100 m of the source. It is also shown that neither ny nor nz can be specified by nw1, the value of n found from a power-law fit to the wind profile in the lowest 8 meters.
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      A PRELIMINARY EVALUATION OF SUTTON'S HYPOTHESIS FOR DIFFUSION FROM A CONTINUOUS POINT SOURCE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150054
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    contributor authorBarad, Morton L.
    contributor authorHaugen, Duane A.
    date accessioned2017-06-09T14:12:02Z
    date available2017-06-09T14:12:02Z
    date copyright1959/02/01
    date issued1959
    identifier issn0095-9634
    identifier otherams-14488.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150054
    description abstractSutton's hypothesis for diffusion from a continuous point source has been evaluated using the data obtained during Project Prairie Grass. It is found that the hypothesis predicts the observed concentration distributions only if there are two values of Sutton's ?n?, one to characterize lateral diffusion (ny) and one to characterize vertical diffusion (nz). Statistical tests indicate that ny and nz are invariant with distance between 100 and 800 m of the source, but that the values of ny and nz appropriate for these distances exceed the values within 100 m of the source. It is also shown that neither ny nor nz can be specified by nw1, the value of n found from a power-law fit to the wind profile in the lowest 8 meters.
    publisherAmerican Meteorological Society
    titleA PRELIMINARY EVALUATION OF SUTTON'S HYPOTHESIS FOR DIFFUSION FROM A CONTINUOUS POINT SOURCE
    typeJournal Paper
    journal volume16
    journal issue1
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1959)016<0012:APEOSH>2.0.CO;2
    journal fristpage12
    journal lastpage20
    treeJournal of Meteorology:;1959:;volume( 016 ):;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