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    Comments on “Lateral Dispersion from Tall Stacks”

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 012::page 1779
    Author:
    Briggs, Gary A.
    DOI: 10.1175/1520-0450(1987)026<1779:CODFTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A few minor errors in a paper by Hanna are noted and several questions are raised about apparent inconsistencies. One question is why substantial enhancement of σy, by buoyancy was noted for the Bull Run data but was unmentioned for the Kincaid data; information given in the paper suggests similar ranges of X*/F* at both plants, but much smaller F* values at Kincaid, which may account for the lack of noticeable buoyancy effects there. The inconsistency between the recommended equation σy/x = 0.6 w*/u and the σy/x values recommended for various stability classes (based on u/w* ranges) can be removed by multiplying this σy expression by a factor which accounts for the effect of mechanical turbulence. Finally, it is noted that an identical equation was recently reported to give a good fit to σy from passive sources released above 0.3 h, albeit to much smaller distances than reported by Hanna.
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      Comments on “Lateral Dispersion from Tall Stacks”

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146489
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    contributor authorBriggs, Gary A.
    date accessioned2017-06-09T14:02:07Z
    date available2017-06-09T14:02:07Z
    date copyright1987/12/01
    date issued1987
    identifier issn0733-3021
    identifier otherams-11279.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146489
    description abstractA few minor errors in a paper by Hanna are noted and several questions are raised about apparent inconsistencies. One question is why substantial enhancement of σy, by buoyancy was noted for the Bull Run data but was unmentioned for the Kincaid data; information given in the paper suggests similar ranges of X*/F* at both plants, but much smaller F* values at Kincaid, which may account for the lack of noticeable buoyancy effects there. The inconsistency between the recommended equation σy/x = 0.6 w*/u and the σy/x values recommended for various stability classes (based on u/w* ranges) can be removed by multiplying this σy expression by a factor which accounts for the effect of mechanical turbulence. Finally, it is noted that an identical equation was recently reported to give a good fit to σy from passive sources released above 0.3 h, albeit to much smaller distances than reported by Hanna.
    publisherAmerican Meteorological Society
    titleComments on “Lateral Dispersion from Tall Stacks”
    typeJournal Paper
    journal volume26
    journal issue12
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1987)026<1779:CODFTS>2.0.CO;2
    journal fristpage1779
    journal lastpage1780
    treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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