学术文献库

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 $0 \leq Λ\leq 1$. The fluid domain is a closed two-dimensional box with aspect ratio $4\leq Γ\leq 16$ and we consider no-slip boundaries and adiabatic side walls. We demonstrate a regime transition from Rayleigh--Bénard convection (RB) to horizontal convection (HC) at $Λ\approx 10^{-2}$, which is independent of $Ra_F$ and $Γ$. At small $Λ$, the flow is organized in multiple overturning cells with approximately unit aspect ratio, while at large $Λ$ 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 $Ra_L=Ra_FΛΓ^4$ are in good agreement with previous results from classical RB convection and HC studies in the limit $Λ\ll 10^{-2}$ and $Λ\gg 10^{-2}$, respectively. We demonstrate that the system is multi-stable near the transition $Λ\approx10^{-2}$, i.e. the exact number of cells not only depends on $Λ$ 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.