2014/03/31 by Céline Guervilly, David W. Hughes, Chris A. Jones · 2 citations
Computer Science · Engineering · Physics and Astronomy · #Combustion and flame dynamics #Convection #Convection cell #Convective heat transfer #Fluid Dynamics and Turbulent Flows #Nonlinear Dynamics and Pattern Formation #Rayleigh number #Reynolds number #Rossby number #Thermal #Vortex #astro-ph.EP #physics.flu-dyn #physics.geo-ph
paper · pdf · doi:10.1017/jfm.2014.542
published as 2014, J. Fluid Mech 758, pp 407-435 · 31 pages, 17 figures, published in J. Fluid Mech
openalex publication_date 2014/10/09 · arxiv created 2014/12/10 · arxiv updated 2014/12/11 · openalex created_date 2016/06/24 · openalex updated_date 2026/08/05
Abstract Using numerical simulations of rapidly rotating Boussinesq convection in a Cartesian box, we study the formation of long-lived, large-scale, depth-invariant coherent structures. These structures, which consist of concentrated cyclones, grow to the horizontal scale of the box, with velocities significantly larger than the convective motions. We vary the rotation rate, the thermal driving and the aspect ratio in order to determine the domain of existence of these large-scale vortices (LSV). We find that two conditions are required for their formation. First, the Rayleigh number, a measure of the thermal driving, must be several times its value at the linear onset of convection; this corresponds to Reynolds numbers, based on the convective velocity and the box depth, \def \xmlpi #1\def \mathsfbi #1\boldsymbol \mathsf #1\let ≤ =\leqslant \let ≤ =\leqslant \let ≥ =\geqslant \let ≥ =\geqslant \def Pr \mathit Pr\def \Fr \mathit Fr\def \Rey \mathit Re\gtrsim 100 . Second, the rotational constraint on the convective structures must be strong. This requires that the local Rossby number, based on the convective velocity and the horizontal convective scale, \lesssim 0.15 . Simulations in which certain wavenumbers are artificially suppressed in spectral space suggest that the LSV are produced by the interactions of small-scale, depth-dependent convective motions. The presence of LSV significantly reduces the efficiency of the convective heat transport.