Wave turbulence on the surface of a fluid in a high-gravity environment
arXiv:1911.04609 · doi:10.1103/PhysRevLett.123.244501
Abstract
We report on the observation of gravity-capillary wave turbulence on the surface of a fluid in a high-gravity environment. By using a large-diameter centrifuge, the effective gravity acceleration is tuned up to 20 times the Earth gravity. The transition frequency between the gravity and capillary regimes is thus increased up to one decade as predicted theoretically. A frequency power-law wave spectrum is observed in each regime and is found to be independent of the gravity level and of the wave steepness. While the timescale separation required by weak turbulence is well verified experimentally regardless of the gravity level, the nonlinear and dissipation timescales are found to be independent of the scale, as a result of the finite size effects of the system (large-scale container modes) that are not taken currently into account theoretically.
in press
References in corpus (5)
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Cited by in corpus (6)
- Experiments in Surface Gravity-Capillary Wave Turbulence
- Experimental quasi-1D capillary-wave turbulence
- Transition from wave turbulence to acousticlike shock-wave regime
- Thermodynamics and Statistical Equilibrium of Large-Scale Hydroelastic Wave Turbulence
- Dynamical large deviations for an inhomogeneous wave kinetic theory: linear wave scattering by a random medium
- Collapse of statistical equilibrium in large-scale hydroelastic turbulent waves