Boundary layers in turbulent vertical convection at high Prandtl number

Abstract

Many environmental flows arise due to natural convection at a vertical surface, from flows in buildings to dissolving ice faces at marine-terminating glaciers. We use three-dimensional direct numerical simulations of a vertical channel with differentially heated walls to investigate such convective, turbulent boundary layers. Through the implementation of a multiple-resolution technique, we are able to perform simulations at a wide range of Prandtl numbers $Pr$. This allows us to distinguish the parameter dependences of the horizontal heat flux and the boundary layer widths in terms of the Rayleigh number $Ra$ and Prandtl number $Pr$. For the considered parameter range $1\le Pr\le 100$, $10^6\le Ra\le 10^9$, we find the flow to be consistent with a 'buoyancy-controlled' regime where the heat flux is independent of the wall separation. For given $Pr$, the heat flux is found to scale linearly with the friction velocity $V_{\ast }$. Finally, we discuss the implications of our results for the parameterisation of heat and salt fluxes at vertical ice-ocean interfaces.

18 pages, 7 figures, submitted to J. Fluid Mech

References in corpus (3)

• Logarithmic temperature profiles in turbulent Rayleigh-Bénard convection
• Regime transitions in thermally driven high-Rayleigh number vertical convection
• The effect of Prandtl number on turbulent sheared thermal convection