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contributor authorDavidson, G. A.
date accessioned2017-06-09T14:01:12Z
date available2017-06-09T14:01:12Z
date copyright1986/06/01
date issued1986
identifier issn0733-3021
identifier otherams-11014.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146196
description abstractOf the numerous integral models that have been developed to describe buoyant plumes in stratified crossflows, Schatzmann's model appears to be the most mathematically rigorous and physically complete. So far, however, a comparative study of the performance of this model with previous simpler integral models has not been reported. To aid such a comparison, a control volume development of Schatzmann's governing equations is presented to parallel his more abstract differential development. Discrepancies between the equation act derived by Schatzmann and that derived from a control volume analysis are reported. The control volume equation act is found to be consistent with the equations published by previous workers, once Schatzmann's suggestion is taken into account that a mean flow convective interaction between the plume and its surroundings be included along with the usual turbulent entrainment interaction. The source of the discrepancies between equation sets is discussed, and a numerical example is presented to illustrate the effect of these differences in the governing equations on plume predictions.
publisherAmerican Meteorological Society
titleA Discussion of Schatzmann's Integral Plume Model from a Control Volume Viewpoint
typeJournal Paper
journal volume25
journal issue6
journal titleJournal of Climate and Applied Meteorology
identifier doi10.1175/1520-0450(1986)025<0858:ADOSIP>2.0.CO;2
journal fristpage858
journal lastpage867
treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 006
contenttypeFulltext


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