Numerical modeling of the global semidiurnal tide in the present day and in the last glacial maximum

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Generation of internal waves in the deep ocean by tides (2005, methodology): “Instead of explicitly correcting for finite depth, as here, the topography was preprocessed with a high-pass filter with a sharp and fixed cutoff at 40 km. (With the method used here, the cutoff varies according to the local depth and stratification.) Egbert et al. [2004] , on the other hand, appea”
The Tides They Are A‐Changin': A Comprehensive Review of Past and Future Nonastronomical Changes in Tides, Their Driving Mechanisms, and Future Implications (2020, methodology): “The effect on the barotropic tide through changes in the internal tide field at regional or global scales has not been well explored beyond sensitivity tests on long time scales (i.e., millennia, see Egbert et al., 2004 and Wilmes & Green, 2014).”
Concurrent Simulation of the Eddying General Circulation and Tides in a Global Ocean Model (2010, unknown): “An iterative procedure appears to be necessary to achieve numerical convergence (e.g. Egbert et al., 2004, AGHS).”
The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, result): “In agreement with other recent studies of global forward tide models (Jayne and St. Laurent, 2001—hereafter JS; Carrere and Lyard, 2003— hereafter CL; Egbert et al., 2004—hereafter ERB), we argue that topographic drag is a plausible mechanism for mid-ocean tidal dissipation.”