Fig. 8: Validation of the model in the case of a water slide with the optimum surface found in Fig. 4 (corresponding to a slide height hs = 1.25h0).
From: On the optimum of the energy transfer efficiency in the generation of waves by subaerial landslides
a sketch of the experimental flume and gauge locations. b temporal evolution of the water surface at the five gauge positions and corresponding simulation results (the dotted red lines mark the times when the signal is affected by the wave reflection on the downstream boundary). c comparison of the camera and model snapshots for different wave breaking stages.
