Observations of turbulence in a tidal beam and across a coastal ridge

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An unstructured-grid, finite-volume, nonhydrostatic, parallel coastal ocean simulator (2006, background): “Lien and Gregg (2001) show that an internal wave beam that is generated at the shelf break just north of the along-canyon transect results in elevated dissipation and mixing.”
The Role of Internal Tides in Mixing the Deep Ocean (2002, unknown): “…be tracked over 1000 km into the central Pacific, though the total internal tide energy flux is only about 2 GW. Microstructure observations have provided direct observations of mixing driven by internal tides at steep topography (Lueck and Mudge 1997; Kunze and Toole 1997; Lien and Gregg 2001).”