Connecting boundary layer dynamics with extreme bulk dissipation events in Rayleigh-Bénard flow

Abstract

We study the connection between extreme events of thermal and kinetic energy dissipation rates in the bulk of three-dimensional Rayleigh-Bénard convection and the wall shear stress patterns at the top and the bottom planes that enclose the layer. Zero points of this two-dimensional vector field stand for detachments of strong thermal plumes. If their position at the opposite planes and a given time is close then they can be considered as precursors for high-amplitude bulk dissipation events triggered by plume collisions or close passings. This scenario requires a breaking of the synchronicity of the boundary layer dynamics at both plates which is found to be in line with a transition of the bulk derivative statistics from Gaussian to intermittent. Our studies are based on three-dimensional high-resolution direct numerical simulations for moderate Rayleigh numbers between $Ra=10^4$ and $5\times 10^5$.

References in corpus (3)

• A Comparison of Turbulent Thermal Convection Between Conditions of Constant Temperature and Constant Flux
• Transitional boundary layers in low-Prandtl-number convection
• Extreme dissipation event due to plume collision in a turbulent convection cell

Cited by in corpus (4)

• Combined particle image velocimetry and thermometry of turbulent superstructures in thermal convection
• Extreme vorticity events in turbulent Rayleigh-Bénard convection from stereoscopic measurements and reservoir computing
• Turbulent mesoscale convection in the Boussinesq limit and beyond
• Three-dimensional velocity gradient statistics in a mesoscale convection laboratory experiment