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Limiting amplitudes of fully nonlinear interfacial tides and solitons

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Figure

Figure 1. The two-fluid layer system for which the forced-MCC-f equations are derived. The horizontal dashed grey line indicates the levelz = 0, the level at which the interface resides at rest.
Figure 2. Amplitude of the linear,and B2); andVarying parameters between panels are L, and quasi-linear, QL, internal tide scaled to the thickness of the upper layer vs
Figure 3. Snapshots of the interfacial displacement of leftward-propagating quasi-linear internal tides for run A1 (LH1 = 30 m;p = 35.49 km)
Figure 4. Snapshots of the interfacial displacement of nonlinear internal tides and solitons in run A1 for a supercritical regime (stages of the nonlinear disintegration of the internal tides
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