Abstract

This work addresses the effects of different thermal sidewall boundary conditions on the formation of flow states and heat transport in two- and three-dimensional Rayleigh–Bénard convection (RBC) by means of direct numerical simulations and steady-state analysis for Rayleigh numbers ${\textit {Ra}}$ up to $4\times 10^{10}$ and Prandtl numbers ${\textit {Pr}}=0.1,1$ and $10$ . We show that a linear temperature profile imposed at the conductive sidewall leads to a premature collapse of the single-roll state, whereas a sidewall maintained at a constant temperature enhances its stability. The collapse is caused by accelerated growth of the corner rolls with two distinct growth rate regimes determined by diffusion or convection for small or large ${\textit {Ra}}$ , respectively. Above the collapse of the single-roll state, we find the emergence of a double-roll state in two-dimensional RBC and a double-toroidal state in three-dimensional cylindrical RBC. These states are most prominent in RBC with conductive sidewalls. The different states are reflected in the global heat transport, so that the different thermal conditions at the sidewall lead to significant differences in the Nusselt number for small to moderate ${\textit {Ra}}$ . However, for larger ${\textit {Ra}}$ , the heat transport and flow dynamics become increasingly alike for different sidewalls and are almost indistinguishable for ${\textit {Ra}}>10^{9}$ . This suggests that the influence of imperfectly insulated sidewalls in RBC experiments is insignificant at very high ${\textit {Ra}}$ – provided that the mean sidewall temperature is controlled.

Highlights

  • Understanding thermally induced convection as it arises in the Earth’s atmospheric/oceanic circulations and deducing its fundamental aspects from laboratory experiments is an ongoing endeavour which motivated numerous experimental and theoretical studies

  • Rayleigh–Bénard convection (RBC), i.e. a fluid held between two parallel plates heated from below and cooled from above, is the most thoroughly investigated model system to study the complex physics behind natural convection such as pattern formation and the transition to turbulence (Bodenschatz, Pesch & Ahlers 2000; Ahlers, Grossmann & Lohse 2009b; Lohse & Xia 2010)

  • We have investigated the influence of three different lateral thermal boundary conditions (BCs), i.e. adiabatic, linearly distributed in the vertical direction and constant ones, on heat transport and flow states in 2-D and 3-D RBC using direct numerical simulation and steady-state analysis

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Summary

Introduction

Understanding thermally induced convection as it arises in the Earth’s atmospheric/oceanic circulations and deducing its fundamental aspects from laboratory experiments is an ongoing endeavour which motivated numerous experimental and theoretical studies. Numerical simulations were performed incorporating thermal conduction in the solid sidewall to clarify the differences between an ideal adiabatic set-up and a finite thermal conductivity sidewall (Verzicco 2002; Stevens, Lohse & Verzicco 2014; Wan et al 2019) The results of these studies suggest that different thermal properties of the sidewall alter the mean flow structure, leading to significant differences in global heat transport in the low to mid Ra range. This effect vanishes for larger Ra, at least when the sidewall temperature is constant and maintained at the arithmetic mean of upper and lower plate temperatures. We first present our numerical methods, discuss the results and conclude with our main findings

Governing equations
Boundary conditions
Adjoint-descent method
Onset of convection
Single roll (states SA1, SL1, SC1 )
Growth of corner rolls The SRS is stable up to a certain Ra limit
Double roll (SA2, SL2)
Direct numerical simulations
Vertical temperature profiles
Vertical sidewall heat flux profiles
Mode analysis
Heat transport
Prandtl number dependence
Conclusions
Derivation
Findings
Choice of the norm
Full Text
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