Shock-capturing non-hydrostatic model for fully dispersive surface wave processes

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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, methodology): “Solutions of the resulting numerical implementation of the Euler equations are usually accurately obtained using only three to five vertical r levels, as shown in MA et al. (2012).”
Numerical simulation of tsunami waves generated by deformable submarine landslides (2013, methodology): “The model we employed in this study is the Non-Hydrostatic WAVE model NHWAVE, which was recently developed by Ma et al. (2012) to study the propagation of fully dispersive, fully nonlinear surface waves in complex 3D coastal environments as well as tsunami wave generation by a prescribed bottom…”
Dispersive tsunami waves in the ocean: Model equations and sensitivity to dispersion and Coriolis effects (2013, methodology): “The non-hydrostatic model NHWAVE (Ma et al., 2012) is used to simulate the first 5 min of tsunami generation, as in Grilli et al. (2012a), using a smaller and finer local 1 km resolution Cartesian grid (see red rectangle in Fig.”