Depth‐integrated, non‐hydrostatic model for wave breaking and run‐up

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Numerical Simulation of the 2011 Tohoku Tsunami Based on a New Transient FEM Co-seismic Source: Comparison to Far- and Near-Field Observations (2013, background): “…studied the effects of the Tohoku tsunami on Hawaii, using two of the early proposed finite-source models obtained from seismic and geodetic inversions (LAY et al. 2011a, b), and applying their ‘‘Non-hydrostatic Evolution of Ocean Wave’’ (NEOWAVE) tsunami propagation model (YAMAZAKI et al. 2009).”
Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up (2010, methodology): “[17] in the spherical coordinate system with dynamic seafloor deformation and implementation of a two-way grid-nesting scheme, which can conform to topographic features for efficient computation of tsunami propagation and coastal run-up.”