Wave–Current Interactions in Finite Depth

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Wave-Current Interaction in an Oceanic Circulation Model with a Vortex-Force Formalism: Application to the Surf Zone (2010, unknown): “However, this assumption has been62 partially falsified in several models with a VF formalism: barotropic models (Smith, 2006; Uchiyama63 et al., 2009), a quasi-3D model (Shi et al., 2006), and 3D models (Newberger and Allen, 2007a,b, called64 “nearshore POM” and designated by NA07, and…”
A global wave parameter database for geophysical applications. Part 1: Wave-current turbulence interaction parameters for the open ocean based on traditional parameterizations (2008, background): “The wave-induced mass transport M = qwTS, where qw is the water density, also comes into the general wave-current interaction equations, whether formulated in terms of the total momentum (Phillips, 1977) or in terms of the mean flow momentum only (Garrett, 1976; Smith, 2006; Ardhuin et al., 2008c).”
A new approach to handle wave breaking in fully non-linear Boussinesq models (2012, background): “It is an important point since the amount of energy dissipated will determine crucial phenomena such as the water level set-up (Bonneton, 2007), and will impact wave-driven circulation (Bonneton et al., 2010; Bühler, 2000; Smith, 2006).”