Neutrally- and Stably-Stratified Boundary Layers Adjustments to a Step Change in Surface Roughness
(2022)
Inverse centrifugal effect induced by collective motion of vortices in rotating thermal convection
Nature Communications Nature Research 12:1 (2021) 5585
Abstract:
AbstractWhen a fluid system is subject to strong rotation, centrifugal fluid motion is expected, i.e., denser (lighter) fluid moves outward (inward) from (toward) the axis of rotation. Here we demonstrate, both experimentally and numerically, the existence of an unexpected outward motion of warm and lighter vortices in rotating thermal convection. This anomalous vortex motion occurs under rapid rotations when the centrifugal buoyancy is sufficiently strong to induce a symmetry-breaking in the vorticity field, i.e., the vorticity of the cold anticyclones overrides that of the warm cyclones. We show that through hydrodynamic interactions the densely distributed vortices can self-aggregate into coherent clusters and exhibit collective motion in this flow regime. Interestingly, the correlation of the vortex velocity fluctuations within a cluster is scale-free, with the correlation length being proportional ( ≈ 30%) to the cluster length. Such long-range correlation leads to the counterintuitive collective outward motion of warm vortices. Our study brings insights into the vortex dynamics that are widely present in nature.Vortices as Brownian particles in turbulent flows.
Science advances 6:34 (2020) eaaz1110
Abstract:
Brownian motion of particles in fluid is the most common form of collective behavior in physical and biological systems. Here, we demonstrate through both experiment and numerical simulation that the movement of vortices in a rotating turbulent convective flow resembles that of inertial Brownian particles, i.e., they initially move ballistically and then diffusively after certain critical time. Moreover, the transition from ballistic to diffusive behaviors is direct, as predicted by Langevin, without first going through the hydrodynamic memory regime. The transitional timescale and the diffusivity of the vortices can be collapsed excellently onto a master curve for all explored parameters. In the spatial domain, however, the vortices exhibit organized structures, as if they are performing tethered random motion. Our results imply that the convective vortices have inertia-induced memory such that their short-term movement can be predicted and their motion can be well described in the framework of Brownian motions.Fine vortex structure and flow transition to the geostrophic regime in rotating Rayleigh-Bénard convection
Physical Review Fluids American Physical Society (APS) 5:1 (2020) 011501
Temperature fluctuations relevant to thermal-plume dynamics in turbulent rotating Rayleigh-Bénard convection
Physical Review Fluids American Physical Society (APS) 4:2 (2019) 023501