Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up

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Dispersive tsunami waves in the ocean: Model equations and sensitivity to dispersion and Coriolis effects (2013, background): “Improvement in model efficiency can be achieved by using nested grids (e.g., Ioualalen et al., 2007; Yamazaki et al., 2011; Son et al., 2011), unstructured or curvilinear grids (Shi et al.”