Influence of the condensate and inverse cascade on the direct cascade in wave turbulence
arXiv:0911.0741 · doi:10.1016/j.matcom.2010.07.009
Abstract
During direct numerical simulation of the isotropic turbulence of surface gravity waves in the framework of Hamiltonian equations formation of the long wave background or condensate was observed. Exponents of the direct cascade spectra at the different levels of an artificial condensate suppression show a tendency to become closer to the prediction of the wave turbulence theory at lower levels of condensate. A simple qualitative explanation of the mechanism of this phenomenon is proposed.
arXiv comment18 pages, 9 figures, submitted to Mathematics and Computers in Simulation
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Cited by in corpus (9)
- Experiments in Surface Gravity-Capillary Wave Turbulence
- Numerical simulation of surface waves instability on a discrete grid
- Inverse cascade of gravity waves in the presence of condensate: numerical simulation
- Saturation of the inverse cascade in surface gravity wave turbulence
- On Dissipation Rate of Ocean Waves due to White Capping
- Direct verification of the kinetic description of wave turbulence for finite-size systems dominated by interactions among groups of 6 waves
- Nonlocal gravity wave turbulence in presence of condensate
- Direct numerical experiment on measuring of dispersion relation for gravity waves in the presence of condensate
- On the applicability of the Hasselmann kinetic equation to the Phillips spectrum