Scaling relations in large-Prandtl-number natural thermal convection
arXiv:1707.07131 · doi:10.1103/PhysRevFluids.2.103502
Abstract
In this study we follow Grossmann and Lohse, Phys. Rev. Lett. 86 (2001), who derived various scalings regimes for the dependence of the Nusselt number and the Reynolds number on the Rayleigh number and the Prandtl number . We focus on theoretical arguments as well as on numerical simulations for the case of large- natural thermal convection. Based on an analysis of self-similarity of the boundary layer equations, we derive that in this case the limiting large- boundary-layer dominated regime is I, introduced and defined in [1], with the scaling relations and . Our direct numerical simulations for from to and from 0.1 to 200 show that the regime I is almost indistinguishable from the regime III, where the kinetic dissipation is bulk-dominated. With increasing , the scaling relations undergo a transition to those in IV of reference [1], where the thermal dissipation is determined by its bulk contribution.
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