Generation of internal tides in an ocean of finite depth: analytical and numerical calculations

By Samar Khatiwala. 2003

175 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory (2010, methodology): “The MITgcm has been used for studies of wave radiation and breaking before (e.g., Khatiwala 2003; Legg and Huijts 2006).”
Internal Wave Breaking at Concave and Convex Continental Slopes (2003, background): “Much recent activity has therefore been focused on understanding where and how this open-ocean component of tidal dissipation occurs (Bell 1975; Baines 1982; Khatiwala 2003; Llewellyn Smith and Young 2002; St. Laurent and Garrett 2002; Polzin 2004).”
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].”
Tidal conversion at a very steep ridge (2003, background): “Analytic (Baines 1973, 1982; Balmforth et al. 2002) and numerical (Holloway & Merrifield 1999; Li 2003; Khatiwala 2003) studies have lifted the weak-topography restriction.”
Energetics of Barotropic and Baroclinic Tides in the Monterey Bay Area (2012, methodology): “This parameter has been used to investigate the role of finite ocean depth on internal wave generation (Llewellyn Smith and Young 2002; Khatiwala 2003; St. Laurent et al. 2003).”
Tidal Conversion by Supercritical Topography (2009, result): “…the internal tide, which can be compared with analogous results for isolated geometries (Llewellyn Smith and Young 2003; St. Laurent et al. 2003; Petrelis et al. 2006), and the numerical simulations of sinusoidal topography (Khatiwala 2003) and isolated steep topography (DiLorenzo et al. 2006).”
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).”
VERTICAL MIXING, ENERGY, AND THE GENERAL CIRCULATION OF THE OCEANS (2004, methodology): “More recent additions to the literature include Balmforth et al. (2002), St. Laurent & Garrett (2002), Llewellyn-Smith & Young (2002), Legg & Adcroft (2003), and Khatiwala (2003).”
Preliminary simulations of internal waves and mixing generated by finite amplitude tidal flow over isolated topography (2006, methodology): “The role of finite ocean depth, as measured by δ = h0/H has been considered by several authors (Llewellyn Smith and Young, 2002; Khatiwala, 2003; St Laurent et al., 2003).”
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Application to the Southern Ocean (2010, background): “However, theories of topographic wave generation have focused on the barotropic tidal component, which is believed to dominate wave radiation in the midlatitudes (e.g., Bell 1975a; Llewellyn Smith and Young 2002; Khatiwala 2003; Garrett and Kunze 2007).”