The study investigates the effects of triad and quartet interactions on the spectral evolution of deep-water surface gravity waves. The authors develop a numerical algorithm to directly track the contributions from quadratic and cubic terms in the dynamical equation, corresponding to triad and quartet interactions, respectively.
The key findings are:
For most wavenumbers, the contributions from triad and quartet interactions show similar magnitude and trend. This is a direct manifestation of the normal form transformation, where the effect of triad interactions is effectively captured at the quartet level.
At low wavenumbers, triad interactions dominate the rapid spectral evolution, leading to a significant energy increase in a short time scale. This is due to the non-resonant nature of triad interactions, which can efficiently distribute energy into the low-energy portion of the spectrum.
Further analysis reveals that the non-resonant triad interactions generate both bound and free modes at the same wavenumber, contrary to the previous understanding that non-resonant interactions only produce bound modes. The authors provide an analytical solution to quantify the energy distribution between the bound and free modes, which is validated through numerical simulations.
Overall, the study demonstrates the important role of triad interactions in shaping the spectral evolution of deep-water surface gravity waves, beyond the commonly considered quartet resonant interactions.
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arxiv.org
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