Short wave amplification and extreme runup by the 2011 Tohoku Tsunami

Optimal dispersion with minimized Poisson equations for non-hydrostatic free surface flows

Importance of horizontal seafloor motion on tsunami height for the 2011 Mw=9.0 Tohoku-Oki earthquake

Improved efficiency of a non-hydrostatic, unstructured grid, finite volume model

A finite volume analogue of the P-1 (NC) - P-1 finite element: with accurate flooding and drying