IG wave generation with 2nd-order correction¶
The wavemaker can take into account bound IG waves based on the weakly-nonlinear second-order finite-depth wave theory of Hasselmann (1962). A time series of wave surface elevation (\(\eta\)) can be described by the linear superposition of free wave components, as in
where \(f_i\) is the frequency and \(\phi_i\) is the phase of \(i^{th}\) wave component. \(N\) is the total number of free wave components. The sub-harmonic component (\(\eta_{ij}\)) generated by two free waves \(i\) and \(j\), is given by
where \(f_{ij} = f_j - f_i\) and \(\phi_{ij}= \phi_j - \phi_i\) (note \(f_j > f_i\)), which represent the frequency and the phase of the sub-harmonic component, respectively. \(D_{ij}\) is the interaction coefficient given by
where \(\omega = 2 \pi f\) is the radial frequency, and \(k_{ij} = k_i - k_j\) is the wave number of the sub-harmonic component. \(C\) is a coefficient given by
The total surface elevation including the sub-harmonics can be described by
where \((n_1, n_2)\) represent the range of free wave components for the sub-harmonic generation. In Li et al. (2020), for example, the range was selected from \(f(n_1)=0.5 f_p\) to \(f(n_2)=1.5 f_p\), where \(f_p\) was the spectral peak frequency. The range selected in Malej (2021) is from \(f(n_1)=0.7 f_p\) to \(f(n_2)=1.3 f_p\), smaller than Li et al. (2020).