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Numerical simulation of cellular convection in air

Published online by Cambridge University Press:  29 March 2006

N. F. Veltishchev
Affiliation:
Hydrometeorological Centre of the U.S.S.R., Moscow
A. A. Zelnin
Affiliation:
Hydrometeorological Centre of the U.S.S.R., Moscow

Abstract

Three-dimensional convection in a Boussinesq fluid confined between horizontal rigid boundaries is studied in a series of numerical experiments. Convection in air, whose Prandtl number Pr = 0·71, is systematically investigated, together with another model for Pr = 1. Convection with a steadily changing mean temperature is also considered. Two-dimensional rolls over the Rayleigh number range 4500 [les ] Ra [les ] 24000 and three-dimensional flow patterns over the range 26000 [les ] Ra ≤ 32000 are shown to be stable in air when the mean temperature of the layer is constant ($\partial \overline{T}/\partial t = \eta = 0$). Discrete changes in the slope of the heat-flux curve are shown to exist in the ranges \[ 7000\leqslant Ra\leqslant 8000,\quad 12000\leqslant Ra\leqslant 14000\quad{\rm and}\quad 24000\leqslant Ra\leqslant 26000 \] in air. Only the last discrete transition in the heat flux is asSociated with a significant transition in the flow pattern. Two-dimensional rolls with a horizontally asymmetric distribution of upward and downward motions over the range 4500 [les ] Ra [les ] 8000, and three-dimensional flow patterns over the range 10 000 [les ] Ra [les ] 20 000 are shown to be stable when the mean temperature varies with time. The circulation in a three-dimensional cell depends on the sign of the mean temperature change: downward motions occupy the centre of the cell when $\partial\overline{T}/\partial t > 0$, and upward motions when $\partial\overline{T}/\partial t < 0 $. Motions start to be time dependent for Ra > 20000. Transitions in the planform are asSociated with discrete changes in the slope of the heat-flux curve. Transitions in both the heat flux and flow pattern depend quantitatively on the Prandtl number.

Type
Research Article
Copyright
© 1975 Cambridge University Press

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References

Brown, W. S. 1973 Heat-flux transitions at low Rayleigh number. J. Fluk.3 Mech. 60, 539559.Google Scholar
Busse, F. H. 1972 The oscillatory instability of convection rolls in a low Prandtl number fluid. J. Fluid Mech. 52, 97112.Google Scholar
Chorin, A. J. 1968 Numerical solution of the Navier-Stokes equations. Math. Comp. 22, 745762.Google Scholar
Krishnamurti, R. 1968a Finite amplitude convection with changing mean temperature. Part 1. Theory. J. Fluid Mech. 33, 445455.Google Scholar
Krishnamurti, R. 1968b Finite amplitude convection with changing mean temperature. Part 2. An experimental test of the theory. J. Fluid Mech. 33, 457463.Google Scholar
Krishnamurti, R. 1970 On the transition to turbulent convection. Part 1. The transition from two-to three-dimensional flow. J. Fluid Mech. 42, 295307.Google Scholar
Krisrnamurti, R. 1973 Some further studies on the transition t turbulent convection. J. Fluid Mech. 60, 285303.Google Scholar
Malkus, W. V. R. 1954 Discrete transitions in turbulent convection. Proc. Roy. Soc. A 225, 185195.Google Scholar
Palm, E. 1960 On the tendency towards hexagonal cells in steady convection. J. Fluid Mech. 8, 183192.Google Scholar
Segel, L. A. 1965 The non-linear interaction of a kite number of disturbances to a layer of fluid heated from below. J. Fluid Mech. 21, 359384.Google Scholar
Segel, L. A. & Stuart, J. T. 1962 On the question of the preferred mode in cellular thermal convection. J. Fluid Mech. 13, 289306.Google Scholar
Somerville, R. C. J. 1973 Numerical simulation of small-scale thermal convection in the atmosphere. In Lecture Notes in Physics, vol. 19, pp. 238245. Springer.Google Scholar
Thirlby, R. 1970 Convection in an internally heated layer. J. Fluid Mech. 44, 673693.Google Scholar
Veltischchev, N. F. 1969 Cellular convection in the atmosphere. Proc. Hydrometeor. Centre Ussr,[dagger] 50, 321.Google Scholar
Veltishchev, N. F. & Želnin, A. A. 1973 Numerical simulation of convection in shear flow. Proc. Hydrometeor. Centre USSR, 110, 3947.Google Scholar
Willis, G. E. & Deardorff, J. W. 1967a Development of short-period temperature fluctuations in thermal convection. Phys. Fluids, 10, 931937.Google Scholar
Willis, G. E. & Deardorff, J. W. 1967b Confirmation and renumbering of the discrete heat flux transitions of Malkus. Phys. Fluids, 10, 18611866.Google Scholar
Willis, G. E. & Deardorff, J. W. 1970 The oscillatory motions of Rayleigh convection. J. Fluid Mech. 44, 661672.Google Scholar
Willis, G. E., Deardorff, J. W. & Somerville, R. C. J. 1972 Roll-diameter dependence in Rayleigh convection and its effect upon the heat flux. J. Fluid Mech. 54, 351367.Google Scholar