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Generation of weakly nonlinear nonhydrostatic internal tides over large topography: a multi-modal approach

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Figure

Fig. 1. The time-development of energy-density for one mode without interaction (a), one mode with self-coupling (b), three modes (c) andten modes (d)
Fig. 2. Comparison of the amplitude of the cross-slope baroclinicvelocity component (in m s−1) from the modal model for 30 modesat the 60th tidal period (upper panel) and a fully numerical model(lower panel)
Fig. 4. The amplitude (in m sgrees, lower panel) of the horizontal cross-slope baroclinic velocitycomponent at the 30th tidal period for 10 modes
Fig. 5. Snapshot of the horizontal cross-slope baroclinic velocity component (in m s−1) for a barotropic tidal forcing increasing from 5 to100 m2 s−1.
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