Transition to the ultimate regime in a radiatively driven convection experiment

Abstract

We report on the transition between two regimes of heat transport in a radiatively driven convection experiment, where a fluid gets heated up within a tunable heating length $\ell$ in the vicinity of the bottom of the tank. The first regime is similar to the one observed in standard Rayleigh-Bénard experiments, the Nusselt number $Nu$ being related to the Rayleigh number $Ra$ through the power-law $Nu\sim R{a}^{1/3}$. The second regime corresponds to the "ultimate" or mixing-length scaling regime of thermal convection, where $Nu$ varies as the square-root of $Ra$. Evidence for these two scaling regimes have been reported in Lepot et al. (Proc. Nat. Acad. Sci. U S A, {\bf 115}, 36, 2018), and we now study in detail how the system transitions from one to the other. We propose a simple model describing radiatively driven convection in the mixing-length regime. \corr{It leads to the scaling relation $Nu\sim \frac{\ell }{H}P{r}^{1/2}R{a}^{1/2}$,} where $H$ is the height of the cell, thereby allowing us to deduce the values of $Ra$ and $Nu$ at which the system transitions from one regime to the other. These predictions are confirmed by the experimental data gathered at various $Ra$ and $\ell$. \corr{We conclude by showing that boundary layer corrections can persistently modify the Prandtl number dependence of $Nu$ at large $Ra$, for $Pr\gtrsim 1$.

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