“…Nonlinear internal waves (hereafter NLIWs) are a ubiquitous oceanic phenomenon in the continental slope region around the world, for example, in the northern South China Sea (Alford et al., 2015; Jia et al., 2021; Klymak et al., 2011), the Oregon continental slope (Martini et al., 2013), the West Shetland slope (Hall et al., 2011, 2013), etc. NLIWs play an important role in mass transport and ocean mixing on continental slopes, through wave transmission, reflection, and breakdown into turbulence (Eriksen, 1982; Gilbert & Garrett, 1989; Munk & Wunsch, 1998; Wunsch, 1968).…”