Heat Transport in the Geostrophic Regime of Rotating Rayleigh-Bénard Convection

Robert E. Ecke and Joseph J. Niemela
Phys. Rev. Lett. 113, 114301 – Published 8 September 2014

Abstract

We report experimental measurements of heat transport in rotating Rayleigh-Bénard convection in a cylindrical convection cell with an aspect ratio of Γ=1/2. The fluid is helium gas with a Prandtl number Pr=0.7. The range of control parameters for Rayleigh numbers 4×109<Ra<4×1011 and for Ekman numbers 2×107<Ek<3×105 (corresponding to Taylor numbers 4×109<Ta<1×1014 and convective Rossby numbers 0.07<Ro<5). We determine the transition from weakly rotating turbulent convection to rotation dominated geostrophic convection through experimental measurements of the heat transport Nu. The heat transport, best collapsed using a parameter RaEkβ with 1.65<β<1.8, defines two boundaries in the phase diagram of Ra/Rac versus Ek and elucidates properties of the geostrophic turbulence regime of rotating thermal convection. We find Nu(Ra/Rac)γ with γ1 from direct measurement and 1.2<γ<1.6 inferred from scaling arguments.

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  • Received 19 August 2013

DOI:https://doi.org/10.1103/PhysRevLett.113.114301

© 2014 American Physical Society

Authors & Affiliations

Robert E. Ecke1,* and Joseph J. Niemela2

  • 1Center for Nonlinear Studies, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
  • 2International Centre for Theoretical Physics, Strada Costiera 11, 34014 Trieste, Italy

  • *Corresponding author. ecke@lanl.gov

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Vol. 113, Iss. 11 — 12 September 2014

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