Boussinesq modeling of longshore currents

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Explicit wave-averaged primitive equations using a generalized Lagrangian mean (2007, background): “A strong nonlinearity combined with a strong current shear and curvature can lead to markedly different wave kinematics (e.g. da Silva and Peregrine 1988).”
Shock-capturing non-hydrostatic model for fully dispersive surface wave processes (2012, methodology): “This data set has been employed by Chen et al. (2003) to test wave-resolving Boussinesq model.”
A high-order adaptive time-stepping TVD solver for Boussinesq modeling of breaking waves and coastal inundation (2012, methodology): “We implemented various boundary conditions including wall boundary condition, absorbing boundary condition following Kirby et al. (1998) and periodic boundary condition following Chen et al. (2003).”
A depth-integrated model for weakly dispersive, turbulent, and rotational fluid flows (2009, unknown): “Chen et al. (2003) eliminated the z dependency by setting z ¼ za in these terms.”
Numerical modeling of tsunami waves generated by the flank collapse of the Cumbre Vieja Volcano (La Palma, Canary Islands): Tsunami source and near field effects (2012, methodology): “FUNWAVE-TVD is a recent extension of the original FUNWAVE code [Wei et al., 1995; Kennedy et al., 2000; Chen et al., 2000, 2003; Kirby, 2003] (see for instance the Appendix in Ioualalen et al. [2007] for a summary to date of FUNWAVE’s equations and numerical methods).”