4.7 Article

On the inverse cascade and flow speed scaling behaviour in rapidly rotating Rayleigh-Benard convection

期刊

JOURNAL OF FLUID MECHANICS
卷 913, 期 -, 页码 -

出版社

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2020.1058

关键词

geostrophic turbulence; quasi-geostrophic flows; turbulent convection

资金

  1. Undergraduate Research Opportunities Program at the University of Colorado, Boulder
  2. National Science Foundation [ACI-1532235, ACI-1532236, 1620649]
  3. University of Colorado Boulder
  4. Colorado State University
  5. Division Of Earth Sciences
  6. Directorate For Geosciences [1620649] Funding Source: National Science Foundation

向作者/读者索取更多资源

The study examines rotating Rayleigh-Benard convection using an asymptotic model that captures rapidly rotating, small Ekman number limit. For sufficiently vigorous convection, the formation of large-scale vortices of opposite polarity is observed. The relative kinetic energy of the large-scale vortices decreases with increasing Rayleigh number, showing a departure from linear scaling at high Rayleigh numbers.
Rotating Rayleigh-Benard convection is investigated numerically with the use of an asymptotic model that captures the rapidly rotating, small Ekman number limit, Ek -> 0. The Prandtl number (Pr) and the asymptotically scaled Rayleigh number ((Ra) over tilde = RaEk(4/3), where Ra is the typical Rayleigh number) are varied systematically. For sufficiently vigorous convection, an inverse kinetic energy cascade leads to the formation of a pair of large-scale vortices of opposite polarity, in agreement with previous studies of rapidly rotating convection. With respect to the kinetic energy, we find a transition from convection dominated states to a state dominated by large-scale vortices at an asymptotically reduced (small-scale) Reynolds number of (Re) over tilde approximate to 6 ((Re) over tilde = ReEk(1/3), where Re is the Reynolds number associated with vertical flows) for all investigated values of Pr. The ratio of the depth-averaged kinetic energy to the kinetic energy of the convection reaches a maximum at (Re) over tilde approximate to 24, then decreases as (Ra) over tilde is increased. This decrease in the relative kinetic energy of the large-scale vortices is associated with a decrease in the convective correlations with increasing Rayleigh number. The scaling behaviour of the convective flow speeds is studied; although a linear scaling of the form (Re) over tilde similar to (Ra) over tilde /Pr is observed over a limited range in Rayleigh number and Prandtl number, a clear departure from this scaling is observed at the highest accessible values of (Ra) over tilde. Calculation of the forces present in the governing equations shows that the ratio of the viscous force to the buoyancy force is an increasing function of (Ra) over tilde, that approaches unity over the investigated range of parameters.

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