“…This procedure is repeated until a pressure equilibrium, that is, a relative pressure of zero, is obtained for every cell at the water surface during the solution cycle of the Reynolds‐averaged Navier–Stokes equations. Previous studies (e.g., Tritthart, Liedermann, & Habersack, ; Krapesch, Tritthart, & Habersack, ; Tritthart, Liedermann, et al, ; Glock et al, ; Glas, Glock, Tritthart, Liedermann, & Habersack, ; Haimann et al, ) have shown good performance of the model RSim‐3D particularly in river applications with associated ecological or sediment‐related research questions.…”