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Propagation of Tsunami-like Surface Long Waves in the Bays of a Variable Depth

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Figure

Fig. 1. Transformation of nonlinear long wave propagating in the bay of model geometry: bottom topography (а) and the structure of the wave field at the following time moments 500 s (b), 1000 s (c), 1500 s (d), 2100 s (e), 2500 s (f), 2900 s (g), 3200 s (h
Fig. 2. Propagation of the nonlinear long wave in the bays with different entrance widths: а, b, c are the moments of the maximum run-up of the wave on the lateral boundary of the bays with the entrance width of 20, 10 and 5 km respectively; d, e, f in the moment of the wave going out of the bays
Fig. 3. Maximal rises of sea level in relation from the initial wavelength in the zones of the largest local amplification: а – in the zone I; b – in the zone II
Fig. 5. Propagation of the long waves in the Feodosiya Gulf(( in the Black Sea: the bottom topography а) and distribution of the sea level displacements in the following instants of time: 200 s (b), 610 s c), 1200 s (d), 1400 s (e), 1550 s (f), 2030 s (g),
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