“…As a result, several attempts have been made to reduce the computational cost, essentially based on socalled thin-layer (or shallow water) depth-averaged models. They have been derived rather precisely for Newtonian flows, and studies for non-Newtonian flows have been proposed in [47,6,7,9,50,25,17,24,45,11,30,31,27,12]. In these works, the approach is most of the time to average the equations (1.1), (1.2) with respect to a variable normal to the bottom topography, and to close the equations by an assumption on the dependency on this normal variable, motivated by observations from natural or experimental flows.…”