“…As such, while we were focused on infinite-depth and finite-depth surface gravity waves due to a moving ship, our analysis can easily be adapted for applications with different dispersion relations. Typical examples that may be of interest include problems for which the effects of surface tension together with gravity are important [23,43,44], models for weakly damped ship waves [45], hydroelastic waves such as those on floating ice sheet [46,47], internal or surface waves due to a stratified fluid [13,48], and ship waves with constant vorticity [21,49] (although further modifications would be required in the latter case due to = (k, ψ )). Our results in Sec.…”