Competition between Rayleigh--B\'enard and horizontal convection

TL;DR

This study explores the transition between Rayleigh--Bénard and horizontal convection in a fluid layer with varying heat flux ratios, revealing a regime change at a specific flux ratio and implications for subglacial lake dynamics.

Contribution

It provides a detailed numerical analysis of the regime transition between RB and HC convection, identifying the critical flux ratio and flow organization changes.

Findings

Regime transition at flux ratio ~10^{-2} independent of other parameters.

Flow organizes into multiple overturning cells at low flux ratio.

Single-cell organization at high flux ratio.

Abstract

We investigate the dynamics of a fluid layer subject to an imposed bottom heat flux and a top monotonically-increasing temperature profile driving horizontal convection. We use direct numerical simulations and consider a large range of flux-based Rayleigh numbers $10^6 \leq Ra_F \leq 10^9$ and imposed top horizontal to bottom vertical heat flux ratios $0 \leq \Lambda \leq 1$. The fluid domain is a closed two-dimensional box with aspect ratio $4\leq \Gamma \leq 16$ and we consider no-slip boundaries and adiabatic side walls. We demonstrate a regime transition from Rayleigh--B\'enard convection (RB) to horizontal convection (HC) at $\Lambda\approx 10^{-2}$, which is independent of $Ra_F$ and $\Gamma$. At small $\Lambda$, the flow is organized in multiple overturning cells with approximately unit aspect ratio, while at large $\Lambda$ a single cell is obtained. The RB-relevant Nusselt number scaling with $Ra_F$ and the HC-relevant Nusselt number scaling with the horizontal Rayleigh number $Ra_L=Ra_F\Lambda\Gamma^4$ are in good agreement with previous results from classical RB convection and HC studies in the limit $\Lambda \ll 10^{-2}$ and $\Lambda \gg 10^{-2}$, respectively. We demonstrate that the system is multi-stable near the transition $\Lambda\approx10^{-2}$, i.e. the exact number of cells not only depends on $\Lambda$ but also on the system's history. Our results suggest that subglacial lakes, which motivated this study, are likely to be dominated by RB convection, unless the slope of the ice-water interface, which controls the horizontal temperature gradient via the pressure-dependence of the freezing point, is greater than unity.