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S. F. Dotsenko (1997)
Numerical analysis of the evolution of tsunami waves in the shelf zone of the South Coast of CrimeaMorsk. Gidrofiz. Zh., 4
E. N. Pelinovsky (1982)
Nonlinear Dynamics of Tsunami Waves
S. Dotsenko (2000)
Analysis of the intensification of tsunami waves near the South Coast of CrimeaPhysical Oceanography, 10
N. E. Voltsinger, K. A. Klevanny, E. N. Pelinovsky (1989)
Long-Wave Dynamics of the Coastal Zone
Y. Shokin, A. Marchuk, L. Chubarov (1979)
To the numerical simulation and propagation of tsunami according to the shallow water equations, 90
T. Murty (1977)
Seismic sea waves: tsunamis
S. F. Dotsenko (1998)
Analysis of the intensification of tsunami waves near the South Coast of CrimeaMorsk. Gidrofiz. Zh., 6
V. A. Magnitsky (1985)
Internal Structure and Physics of the Earth
N. E. Voltsinger, R. V. Pyaskovsky (1968)
Basic Oceanological Problems of the Theory of Shallow Water
S. F. Dotsenko (1998)
Evaluation of the level of tsunami danger for the Black SeaVestnik Mosk. Univ. Ser. 3. Fiz., Astron., 4
Yu. I. Shokin, L. B. Chubarov, An. G. Marchuk, K. V. Simonov (1969)
Numerical Experiments in the Problem of Tsunami
An. G. Marchuk, L. B. Chubarov, Yu. I. Shokin (1983)
Numerical Simulation of Tsunami Waves
A. A. Nikonov (1997)
Tsunami on the coasts of the Black Sea and Sea of AzovIzv. Ross. Akad. Nauk. Fiz. Zemli, 1
S. F. Dotsenko (1997)
Numerical simulation of the propagation of tsunami in the shelf zone of the Crimean PeninsulaMorsk. Gidrofiz. Zh., 5
S. L. Solov’ev, Ch. N. Go (1974)
A Catalogue of Tsunami for the Western Coast of the Pacific Ocean
L. V. Cherkesov (1973)
Surface and Internal Waves
We perform the analysis of tsunami waves in the shelf zone of the Crimean peninsula generated by underwater earthquakes whose epicentres are located near the lower boundary of the continental slope. For this purpose, we use a one-dimensional nonlinear dissipative numerical model of long waves. The investigated distributions of the depth of the basin correspond to four points of the south coast of the Crimean peninsula. We use the empirical dependences of parameters of the sources of tsunami waves on the magnitude of the earthquake obtained earlier for the Pacific Ocean. It is shown that the height, vertical climb, and duration of tsunami waves increase with the magnitude of the earthquake. For equal magnitudes of the earthquake, the highest tsunamis on the south coast of the Crimea are observed between Alushta and Yalta. We also deduced a generalized regression dependence of the height of tsunami waves near the coast on the magnitude of the earthquake.
Physical Oceanography – Springer Journals
Published: Sep 18, 2006
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