Tidal conversion at a very steep ridge

By Stefan G. Llewellyn Smith, William R. Young. Journal of Fluid Mechanics, 2003

134 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Direct Breaking of the Internal Tide near Topography: Kaena Ridge, Hawaii (2008, unknown): “Using linear tide generation models this is proportional to U2 (St. Laurent and Garrett 2002; Llewellyn Smith and Young 2003).”
Preliminary simulations of internal waves and mixing generated by finite amplitude tidal flow over isolated topography (2006, background): “For steep slopes and deep fluid, energy conversion is enhanced by a factor 2, relative to predictions made assuming subcritical slopes (St Laurent et al., 2003; Llewellyn Smith and Young, 2003).”
Generation of internal waves in the deep ocean by tides (2005, background): “Laurent et al., 2003; Balmforth et al., 2002; Llewellyn Smith and Young, 2003; Khatiwala, 2003; J. Nycander, Tidal generation of internal waves from a periodic array of steep ridges, submitted to Journal of Fluid Mechanics, 2005, hereinafter referred to as Nycander, submitted manuscript, 2005].”
The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, background): “…and Tierney (1997), Holloway and Merrifield (1999), Kang et al. (2000), Merrifield et al. (2001), Niwa and Hibiya (2001), Balmforth et al. (2002), St. Laurent and Garrett (2002), Llewellyn Smith and Young (2002, 2003), Khatiwala (2003), St. Laurent et al. (2003), Legg (2004), and Polzin (2004).”
Global Abyssal Mixing Inferred from Lowered ADCP Shear and CTD Strain Profiles (2006, background): “Turbulent mixing of 100–1000 times the ocean interior values is found over seamounts (Nabatov and Ozmidov 1988; Kunze and Toole 1997; Lueck and Mudge 1997), ridges (Althaus et al. 2003; Klymak et al. 2006), canyons (St. Laurent et al. 2001; Carter and Gregg 2002), and hydraulically controlled…”
Tidal Conversion by Supercritical Topography (2009, background): “For the more widely separated obstacles (g 5 4 and higher), the conversion rate initially flattens out close to 2 before the beginning of the interference sequence, which is the value expected for an isolated knife edge (Llewellyn Smith and Young 2003; Nycander 2006).”