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contributor authorDeardorff, J. W.
date accessioned2017-06-09T14:13:34Z
date available2017-06-09T14:13:34Z
date copyright1965/07/01
date issued1965
identifier issn0022-4928
identifier otherams-15111.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150748
description abstractA numerical model for the study of three-dimensional, small-scale, horizontally homogeneous turbulence is presented for use with a two-dimensional grid in a vertical plane. The model is called pseudo three-dimensional because all quantities involving one of the horizontal dimensions are obtained by assumption during the calculations. It is applied to the problem of turbulent thermal convection between horizontal plates, with a Rayleigh number of 6.75?105, and Prandtl numbers of 0.71 and 10. It is shown that this model allows turbulent motions to develop, whereas a two-dimensional model yields nearly steady convective rolls. The calculated heat flux is only about 5 per cent larger than experimental values, and the horizontal variances of temperature, vertical velocity and horizontal velocity are in rough agreement with observations at all levels. Terms in the vorticity and temperature variance equations are also evaluated, although experimental values are lacking for comparison.
publisherAmerican Meteorological Society
titleA Numerical Study of Pseudo Three-Dimensional Parallel-Plate Convection
typeJournal Paper
journal volume22
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1965)022<0419:ANSOPT>2.0.CO;2
journal fristpage419
journal lastpage435
treeJournal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 004
contenttypeFulltext


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