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Experimental results on a rip formed over a heterogeneous beach with a mobile sandy bed are analyzed using a 2D depth-averaged Non Linear Shallow Water Equations (NSWE) model. The numerical model is validated comparing results with measured wave height va

A quantitative theory of the elastic wave damping and velocity change due to interaction with dislocations is presented. It provides a firm theoretical basis and a generalization of the Granato and Lücke model [J. Appl. Phys. 27, 583 (1956)]. This is done