Scaling of large-scale quantities in Rayleigh-Bénard convection
arXiv:1611.09071 · doi:10.1063/1.4962307
Abstract
We derive a formula for the Péclet number () by estimating the relative strengths of various terms of the momentum equation. Using direct numerical simulations in three dimensions we show that in the turbulent regime, the fluid acceleration is dominated by the pressure gradient, with relatively small contributions arising from the buoyancy and the viscous term, in the viscous regime, acceleration is very small due to a balance between the buoyancy and the viscous term. Our formula for describes the past experiments and numerical data quite well. We also show that the ratio of the nonlinear term and the viscous term is , where and are Reynolds and Rayleigh numbers respectively, and that the viscous dissipation rate , where is the root mean square velocity and is the distance between the two horizontal plates. The aforementioned decrease in nonlinearity compared to free turbulence arises due to the wall effects.
arXiv comment35 pages, 15 figures
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