Abstract
From the observed behaviour of free convection at high Rayleigh number above a horizontal surface, a simple model of the temperature profile in such a region is constructed. This model is used to predict the gross properties of a layer of fluid which is heated from below. At the top boundary, the effect of replacing a rigid insulated surface by a stable layer of fluid (that is a temperature inversion) is considered. The behaviour of the region is found to depend strongly upon the boundary conditions at the base and at the top of the convection layer.
Similar content being viewed by others
References
Somerscales, E. F. C. and I. W. Gazda, Int. J. Heat Mass Trans. 12 (1969) 1491.
Warner, J. and J. W. Telford, J. Atmos. Sci. 24 (1967) 374.
Jakob, M., Trans. A.S.M.E. 68 (1946) 189.
Spiegel, E. A. Ann. Rev. Aston. Astrophys. 9 (1971) 323.
Howard, L. N., Proc. 11th Int. Cong. Appl. Mech. (ed. H. Gortler) Springer, 1966.
Sparrow, E. M., R. B. Husar and R. J. Goldstein, J. Fluid Mech. 41 (1970) 793.
Ball, F. K., Quart. J. Roy. Meteor. Soc. 86 (1960) 483.
Tennekes, H., J. Atmos. Sci. 30 (1973) 558.
Abramowitz, M. and I. A. Stegun, Handbook of Mathematical Functions, Dover, N.Y., 1965.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Manton, M.J. On the high Rayleigh number heating of a fluid above a horizontal surface. Appl. Sci. Res. 31, 267–278 (1975). https://doi.org/10.1007/BF00389219
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF00389219