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contributor authorO'Brien, Edward E.
date accessioned2017-06-09T14:13:50Z
date available2017-06-09T14:13:50Z
date copyright1966/07/01
date issued1966
identifier issn0022-4928
identifier otherams-15211.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150859
description abstractUnder the assumption that the detailed turbulence structure in the constant-stress region of a fluid flowing over a rough wall is in a universal state determined wholly by the friction velocity u* a similarity analysis of a Lagrangian type can be applied to the relative dispersion of clouds of contaminant released in such a layer. It is found that for the case in which the initial dimension of the cloud, say L, and the initial mean height are comparable, there are only two temporal regimes and they are characterized by times smaller than or greater than L/u*. For the small time regime all relative diffusivities are linearly dependent on time and their directional properties are related to Eulerian measurements. Of more interest are the predictions in the long time regime. It is also found in this region that relative diffusion is characterized by a diffusivity that is linearly dependent on time. Such a prediction differs from that of homogeneous turbulence and seems to have some support from experimental data in the earth's atmosphere.
publisherAmerican Meteorological Society
titleDiffusion of Clouds of Contaminant in a Turbulent Boundary Layer
typeJournal Paper
journal volume23
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1966)023<0387:DOCOCI>2.0.CO;2
journal fristpage387
journal lastpage389
treeJournal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 004
contenttypeFulltext


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