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The large-scale flow structure in turbulent rotating Rayleigh–Bénard convection

Published online by Cambridge University Press:  01 November 2011

Stephan Weiss
Affiliation:
Department of Physics, University of California, Santa Barbara, CA 93106, USA
Guenter Ahlers*
Affiliation:
Department of Physics, University of California, Santa Barbara, CA 93106, USA
*
Email address for correspondence: guenter@physics.ucsb.edu

Abstract

We report on the influence of rotation about a vertical axis on the large-scale circulation (LSC) of turbulent Rayleigh–Bénard convection in a cylindrical vessel with aspect ratio (where is the diameter and the height of the sample). The working fluid is water at an average temperature with a Prandtl number . For rotation rates , corresponding to inverse Rossby numbers between 0 and 20, we investigated the temperature distribution at the sidewall and from it deduced properties of the LSC. The work covered the Rayleigh-number range . We measured the vertical sidewall temperature gradient, the dynamics of the LSC and flow-mode transitions from single-roll states (SRSs) to double-roll states (DRSs). We found that modest rotation stabilizes the SRSs. For modest we found the unexpected result that the vertical LSC plane rotated in the prograde direction (i.e. faster than the sample chamber), with the rotation at the horizontal midplane faster than near the top and bottom. This differential rotation led to disruptive events called half-turns, where the plane of the top or bottom section of the LSC underwent a rotation through an angle of relative to the main portion of the LSC. The signature of the LSC persisted even for large where Ekman vortices are expected. We consider the possibility that this signature actually is generated by a two-vortex state rather than by a LSC. Whenever possible, we compare our results with those for a sample by Zhong & Ahlers (J. Fluid Mech., vol. 665, 2010, pp. 300–333).

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Copyright © Cambridge University Press 2011

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