Tidal Conversion by Supercritical Topography

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Energetics of M2 Barotropic-to-Baroclinic Tidal Conversion at the Hawaiian Islands (2008, background): “2006), but their formation is dependent on the criticality of the local slope (Balmforth et al. 2002; Garrett and Kunze 2007).”
Energetics of Barotropic and Baroclinic Tides in the Monterey Bay Area (2012, background): “…lost to (modeled) dissipation and mixing. c. Comparison to linear theory A number of theoretical estimates of tidal energy conversion have been presented in previous studies (Bell 1975; Llewellyn Smith and Young 2002; Balmforth et al. 2002; St. Laurent et al. 2003; Balmforth and Peacock 2009).”
On the generation and evolution of nonlinear internal waves in the South China Sea (2010, background): “[9] Slopes featuring g 1 are subcritical, critical,andsupercritical,respectively.Atcriticalslopeswelldefined internal wave beams are formed [ Balmforth et al., 2002 ].”