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dc.contributor.authorBriggs, Gary A.
dc.date.accessioned2017-06-09T14:02:07Z
dc.date.available2017-06-09T14:02:07Z
dc.date.copyright1987/12/01
dc.date.issued1987
dc.identifier.issn0733-3021
dc.identifier.otherams-11279.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146489
dc.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.
dc.publisherAmerican Meteorological Society
dc.titleComments on “Lateral Dispersion from Tall Stacks”
dc.typeJournal Paper
dc.journal.volume26
dc.journal.issue12
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1987)026<1779:CODFTS>2.0.CO;2
dc.journal.fristpage1779
dc.journal.lastpage1780
dc.treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 012
dc.contenttypeFulltext


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