Excitation of interfacial waves via near---resonant surface---interfacial wave interactions
arXiv:1904.08329 · doi:10.1017/jfm.2019.1033
Abstract
We consider interactions between surface and interfacial waves in the two layer system. Our approach is based on the Hamiltonian structure of the equations of motion, and includes the general procedure for diagonalization of the quadratic part of the Hamiltonian. Such diagonalization allows us to derive the interaction crossection between surface and interfacial waves and to derive the coupled kinetic equations describing spectral energy transfers in this system. Our kinetic equation allows resonant and near resonant interactions. We find that the energy transfers are dominated by the class III resonances of \cite{Alam}. We apply our formalism to calculate the rate of growth for interfacial waves for different values of the wind velocity. Using our kinetic equation, we also consider the energy transfer from the wind generated surface waves to interfacial waves for the case when the spectrum of the surface waves is given by the JONSWAP spectrum and interfacial waves are initially absent. We find that such energy transfer can occur along a timescale of hours; there is a range of wind speeds for the most effective energy transfer at approximately the wind speed corresponding to white capping of the sea. Furthermore, interfacial waves oblique to the direction of the wind are also generated.
References in corpus (9)
- Toward Regional Characterizations of the Oceanic Internal Wavefield
- Hamiltonian formalism and the Garrett-Munk spectrum of internal waves in the ocean
- Statistical Description of Acoustic Turbulence
- Energy spectra of the ocean's internal wave field: theory and observations
- Joint statistics of amplitudes and phases in Wave Turbulence
- "Noisy" spectra, long correlations and intermittency in wave turbulence
- Anomalous probability of large amplitudes in wave turbulence
- A Hamiltonian Formulation for Long Internal Waves
- Nonlinear wave-wave interactions in stratified flows: Direct numerical simulations