Abstract
Horizontal convection is studied numerically in two dimensions for the case of an infinite Prandtl number and shear-free boundary conditions on all sides. Three different temperature distributions are applied at the top boundary. Steady states become unstable, giving way to unsteady flow with increasing Rayleigh number Ra. The transition to time-varying flow depends on the heating configuration. For simulations show a time-dependent flow behavior for a linearly varying temperature at the top, whereas other temperature distributions show this transition at even lower Rayleigh numbers. The scaling laws of heat flow and circulation strength are investigated and the results indicate that both are changed by the upcoming time-dependent flow. While in the steady boundary layer flow regime the heat flux scales as , the exponent increases to a value of approximately in the unsteady regime. A similar transition is observed for the circulation strength. The observed scaling laws are in good agreement with established theories in both the steady and unsteady regimes. After the transition, the flow shows a periodic oscillation of the boundary layer circulation, which turns into a more irregular flow behavior as the Rayleigh number is increased further. We conclude that, even for an infinite Prandtl number, horizontal convection exhibits unsteady flow at sufficiently high Rayleigh numbers and that this flow resembles the turbulent circulation at low Prandtl numbers.
- Received 17 March 2019
DOI:https://doi.org/10.1103/PhysRevFluids.4.093501
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