Semi‐diurnal and diurnal tidal dissipation from TOPEX/Poseidon altimetry

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Spatial and temporal variability of global ocean mixing inferred from Argo profiles (2012, background): “Other notable examples of elevated dissipation rates in Figure 1 that also exhibit high tidal kinetic energy [Egbert and Ray, 2003] include the North Madagascar Ridge, the Southeast Bay of Bengal, the Aleutian Ridge, the Izu-Ogasawara-Mariana Ridge, South Georgia Ridge, the ridges north and south…”
Prototypical solitons in the South China Sea (2006, background): “Inverse modelling indicates that the diurnal component of energy may be larger than the semi-diurnal [Egbert and Ray, 2003].”
Modeling climate diversity, tidal dynamics and the fate of volatiles on TRAPPIST-1 planets (2017, background): “On Earth, the dissipation is dominated by the dynamical response of the ocean and friction processes along the costline and to a lesser extent to interactions with seafloor topography in deep ocean (Egbert & Ray 2000, 2003; Williams et al. 2014).”