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contributor authorGrant, Alison M.
date accessioned2017-06-09T14:11:39Z
date available2017-06-09T14:11:39Z
date copyright1957/08/01
date issued1957
identifier issn0095-9634
identifier otherams-14350.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149902
description abstractThe results of the conventional mixing-length theory disagree with those of the statistical theory of turbulence, and must be rejected also on common-sense grounds since they imply the existence of infinite velocities. This does not result from any lack of realism on the part of the basic assumptions of the mixing-length theory, but from an inconsistency in their application, namely the implicit assumption that fluid parcels can travel the entire distance between ?collisions? during an infinitesimal dispersion time, although they are explicitly assumed to travel with a finite velocity. Removal of this inconsistency leads to a corrected theory whose results are in agreement with those of the statistical theory. The corrected theory, which yields a diffusion equation with the coefficient K varying with dispersion time, also provides a description of the diffusion for all dispersion times in terms of the energy spectrum of eddy lifetimes. The criticism of the conventional mixing-length theory is shown to apply also to the classical theory of molecular diffusion, so that there can be no theoretical justification for the simple diffusion equation with K independent of the dispersion time. The implications of the corrected theory for atmospheric diffusion are discussed qualitatively, the diffusion of smoke from a source at ground level being taken as an example.
publisherAmerican Meteorological Society
titleA CORRECTED MIXING-LENGTH THEORY OF TURBULENT DIFFUSION
typeJournal Paper
journal volume14
journal issue4
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1957)014<0297:ACMLTO>2.0.CO;2
journal fristpage297
journal lastpage303
treeJournal of Meteorology:;1957:;volume( 014 ):;issue: 004
contenttypeFulltext


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