paper

Steady Rayleigh--Bénard convection between no-slip boundaries

arXiv:2008.08752 · doi:10.1017/jfm.2021.1042

Abstract

The central open question about Rayleigh--Bénard convection -- buoyancy-driven flow in a fluid layer heated from below and cooled from above -- is how vertical heat flux depends on the imposed temperature gradient in the strongly nonlinear regime where the flows are typically turbulent. The quantitative challenge is to determine how the Nusselt number depends on the Rayleigh number in the limit for fluids of fixed finite Prandtl number in fixed spatial domains. Laboratory experiments, numerical simulations, and analysis of Rayleigh's mathematical model have yet to rule out either of the proposed `classical' or `ultimate' asymptotic scaling theories. Among the many solutions of the equations of motion at high are steady convection rolls that are dynamically unstable but share features of the turbulent attractor. We have computed these steady solutions for up to with and various horizontal periods. By choosing the horizontal period of these rolls at each to maximize , we find that steady convection rolls achieve classical asymptotic scaling. Moreover, they transport more heat than turbulent convection in experiments or simulations at comparable parameters. If heat transport in turbulent convection continues to be dominated by heat transport in steady rolls as , it cannot achieve the ultimate scaling.

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