“…Instead, they observed a growing horizontal mean flow of the streaming type which also impacts the beam itself via refraction. This induced mean flow is of viscous origin and hinges on the combined effects of transverse variations and nonlinearity (Kataoka & Akylas 2015;Fan, Kataoka & Akylas 2018;Jamin et al 2020). However, as noted by Dauxois et al (2018), it is unclear whether streaming and TRI can coexist, and the conditions that would favour one over the other remain largely unexplored.…”