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dc.contributor.authorSchatzmann, M.
dc.contributor.authorPolicastro, A. J.
dc.date.accessioned2017-06-09T13:59:56Z
dc.date.available2017-06-09T13:59:56Z
dc.date.copyright1984/01/01
dc.date.issued1984
dc.identifier.issn0733-3021
dc.identifier.otherams-10644.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145784
dc.description.abstractNearly all mathematical models which are commonly used to predict the dispersion of chimney gases in the atmosphere or heated water discharges in the aquatic environment employ the so-called Boussinesq approximation. It is part of this approximation that density variations appear solely in the buoyancy term of the momentum equation and are neglected in all other terms. The exact limits of validity of the Boussinesq approximation and the precise effects the simplifications have on model performance are known only qualitatively. The objective of this paper is to present, for a variety of industrial stack plumes with different initial density ratios, comparisons of predictions which have been obtained employing 1) a model which makes the Boussinesq approximation and 2) a version of the same model in which this approximation has not been introduced. It was found that the difference in jet-property predictions between the two models increases with increasing initial density defect ratio. In the case of the largest ratio tested (??/?∞= 0.5), the maximum height of rise predicted with the Boussinesq approximated model was ?20% larger than predicted with the non-Boussinesq approximated model. These differences in predictions are, of course, to some extent model-specific but provide, nevertheless, a first quantitative estimate on how the Boussinesq approximation affects the performance of plume models.
dc.publisherAmerican Meteorological Society
dc.titleEffects of the Boussinesq Approximation on the Results of Strongly-Buoyant Plume Calculations
dc.typeJournal Paper
dc.journal.volume23
dc.journal.issue1
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1984)023<0117:EOTBAO>2.0.CO;2
dc.journal.fristpage117
dc.journal.lastpage123
dc.treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 001
dc.contenttypeFulltext


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