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Application of a Сhannel Model for Describing Propagation of Tsunami-Like Single Waves in a Channel with Variable Cross-Section

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Figure

Fig. 1. The Bosporus with an indication of the positions of 54 cross-sections and the depth distributions (on the sidebar) in sections 2, 25, 35 and 42
Fig. 2.PHYSICAL OCEANOGRAPHY   NO. 1 (2015)  Distributions along the Bosporus axis of the maximum depth (а), mirror half-width (b) and cross-section areas (c) 31
Fig. 3. 3 The change along the strait axis of the maximum possible heights of waves propagating from the Marmara to the Black Sea (a) and from the Black Sea to the Marmara (b) at various initial wavelengths: 1 – calculation according to the approximate formula below (18); 2 – λ  = 0.5 km;  –λ  = 1 km; 4 –λ  = 2 km; 5 –λ  = 5 km; 6 –λ  = 10 km (initial wave height is 1 m)
Fig. 4.34 the Marmara (formula (19); velocities in the waves propagating from the Marmara to the Black Sea ( Change along the strait axis of the maximum 2 b) for different lengths of the entering wave: –λ  = 0.5 km; 3 –λ  = 1 km; 4 –λ  = 2 km;PHYSICAL OCEA
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