The cause of oscillations of the large-scale circulation of turbulent Rayleigh-B{\'e}nard convection

TL;DR

This paper investigates the oscillatory behavior of the large-scale circulation in turbulent Rayleigh-Bénard convection, identifying a sloshing mode and extending a model to explain its dynamics and restoring forces.

Contribution

It extends previous models to include lateral displacements and height variations, accurately predicting oscillation characteristics in turbulent convection.

Findings

Confirmed the existence of a sloshing mode matching experimental observations.

Extended the model to include lateral displacements and height variations.

Predicted oscillation frequency, phase, and displacement distributions accurately.

Abstract

In agreement with a recent experimental discovery by Xia et. al. (2009), we also find a sloshing mode in experiments on the large-scale circulation (LSC) of turbulent Rayleigh-Benard convection in a cylindrical sample of aspect ratio one. The sloshing mode has the same frequency as the torsional oscillation discovered by Funfschilling and Ahlers (2004). We show that both modes can be described by an extension of a model developed previously [Brown and Ahlers (2008)] which consists of permitting a lateral displacement of the LSC circulation plane away from the vertical center line of the sample as well as a variation in displacements with height (such displacements had been excluded in the original model). Pressure gradients produced by the side wall of the container on average center the plane of the LSC so that it prefers to reach its longest diameter. If the LSC is displaced away from this diameter, the walls provide a restoring force. Turbulent fluctuations drive the LSC away from the central alignment, and combined with the restoring force they lead to oscillations. These oscillations are advected along with the LSC. This model predicts the correct wavenumber and phase of the oscillations, as well as estimates of the frequency, amplitude, and probability distributions of the displacements.