Ultimate-state scaling in a shell model for homogeneous turbulent convection
Emily S.C. Ching, T.C. Ko

TL;DR
This paper investigates the scaling laws of heat transport and flow velocity in turbulent convection using a shell model, revealing that the ultimate state may not be bulk-dominated if buoyancy acts on most scales.
Contribution
It introduces a shell model analysis showing that the ultimate state scaling arises with large-scale drag, challenging the bulk-dominated interpretation.
Findings
Nu scales as Ra^{1/2} Pr^{1/2}
Re scales as Ra^{1/2} Pr^{-1/2}
Large-scale drag influences ultimate-state scaling
Abstract
An interesting question in turbulent convection is how the heat transport depends on the strength of thermal forcing in the limit of very large thermal forcing. Kraichnan predicted [Phys. Fluids {\bf 5}, 1374 (1962)] that the heat transport measured by the Nusselt number (Nu) would depend on the strength of thermal forcing measured by the Rayleigh number (Ra) as Nu Ra with possible logarithmic corrections at very high Ra. This scaling behavior is taken as a signature of the so-called ultimate state of turbulent convection. The ultimate state was interpreted in the Grossmann-Lohse (GL) theory [J. Fluid Mech. {\bf 407}, 27 (2000)] as a bulk-dominated state in which both the kinetic and thermal dissipation are dominated by contributions from the bulk of the flow with the boundary layers either broken down or playing no role in the heat transport. In this paper, we study the…
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