Abstract

In the problem of horizontal convection a non-uniform buoyancy, , is imposed on the top surface of a container and all other surfaces are insulating. Horizontal convection produces a net horizontal flux of buoyancy, , defined by vertically and temporally averaging the interior horizontal flux of buoyancy. We show that ; the overbar denotes a space–time average over the top surface, angle brackets denote a volume–time average and is the molecular diffusivity of buoyancy . This connection between and justifies the definition of the horizontal-convective Nusselt number, , as the ratio of to the corresponding quantity produced by molecular diffusion alone. We discuss the advantages of this definition of over other definitions of horizontal-convective Nusselt number. We investigate transient effects and show that equilibrates more rapidly than other global averages, such as the averaged kinetic energy and bottom buoyancy. We show that is the volume-averaged rate of Boussinesq entropy production within the enclosure. In statistical steady state, the interior entropy production is balanced by a flux through the top surface. This leads to an equivalent ‘surface Nusselt number’, defined as the surface average of vertical buoyancy flux through the top surface times the imposed surface buoyancy . In experimental situations it is easier to evaluate the surface entropy flux, rather than the volume integral of demanded by .

Highlights

  • Horizontal convection (HC) is convection generated in a fluid layer 0 < z < h by imposing non-uniform buoyancy along the top surface z = h; all other bounding894 A24-2 C

  • We show that κ |∇b|2 is the volume-averaged rate of Boussinesq entropy production within the enclosure

  • In the context of Rayleigh–Bénard convection (RBC), Howard (1963) remarked that χ is a measure of the entropy production by thermal diffusion within the enclosure; in this work, we explore the ramifications of viewing (1.1) as a measure of HC entropy production

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Summary

Introduction

In RBC the correct definition of the Nusselt number, Nu, is clear: after averaging over (x, y, t) there is a constant vertical heat flux passing through every level of constant z between 0 and h. To obtain a non-zero index of the vertical heat flux, Rossby (1965, 1998) defined the Nusselt number of HC as a suitably normalized version of |F|. This justifies referring to χ /χdiff as a Nusselt number, and we note other advantages that compel (1.1) as the best definition of a horizontal-convective Nusselt number.

Formulation of the HC problem
Horizontal-convective boundary conditions and control parameters
Horizontal-convective power integrals
Definition of the horizontal-convective Nusselt number
The Nusselt number
The Nusselt number of a discontinuous surface buoyancy profile
Two-dimensional surface buoyancy distributions and the effective diffusivity
Entropy production and surface entropy flux
Equilibration of the Nusselt number
The surface Nusselt number Nus
The Nusselt number NuF and its relation to Nu and Nus
Conclusion
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