“…For instance, two of the three system eigenvalues vanish [60], which requires a careful treatment of critical conditions and the absence of sediment motion. Schemes used for strongly coupled or decoupled numerical schemes are also the object of intense debates [29,45,66,72]. Interestingly here, we will see that the erosiondeposition formulation for bed load transport allows us to readily extend previous finite volume methods for frictional shallow water equations similar to what has been done for computing the suspended load in dilute flows, see Bohorquez and Fernández-Feria [14].…”