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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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