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Turbulent rotating convection: an experimental study

Published online by Cambridge University Press:  30 May 2002

PETER VOROBIEFF  and
ROBERT E. ECKE
PETER VOROBIEFF
Affiliation:
Department of Mechanical Engineering, University of New Mexico, Albuquerque, NM 87131, USA CNLS/MST-10, MS K-764, Los Alamos National Laboratory, Los Alamos, NM 87545, USA
ROBERT E. ECKE
Affiliation:
CNLS/MST-10, MS K-764, Los Alamos National Laboratory, Los Alamos, NM 87545, USA
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Abstract

We present experimental measurements of velocity and temperature fields in horizontal planes crossing a cylindrical Rayleigh–Bénard convection cell in steady rotation about its vertical axis. The range of dimensionless rotation rates Ω is from zero to 5×104 for a Rayleigh number R = 3.2×108. The corresponding range of convective Rossby numbers is ∞ > Ro > 0.06. The patterns of velocity and temperature and the flow statistics characterize three basic flow regimes. For Ro [Gt ] 1, the flow is dominated by vortex sheets (plumes) typical of turbulent convection without rotation. The flow patterns for Ro ∼ 1 are cyclone-dominated, with anticyclonic vortices rare. As the Rossby number continues to decrease, the number of anticyclonic vortex structures begins to grow but the vorticity PDF in the vicinity of the top boundary layer still shows skewness favouring cyclonic vorticity. Velocity-averaging near the top of the cell suggests the existence of a global circulation pattern for Ro [Gt ] 1.

Type
Research Article
Information
Journal of Fluid Mechanics , Volume 458 , 10 May 2002 , pp. 191 - 218
Copyright
© 2002 Cambridge University Press

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