Workshop On Renormalization Group, Kyoto 2005 B. Tirozzi, S.Yu. Dobrokhotov, S.Ya. Sekerzh-Zenkovich, T.Ya. Tudorovskiy Analytical and numerical analysis of the wave profiles near the fronts appearing in Tsunami problems
“Gaussian” source of Earthquake
Level curves of perturbation
Wave profiles at the front at time t at different angles
3D wave profile for elliptic source
“Modulated gaussian” source of Earthquake
Level curves of perturbation
Wave profiles at the front at time t at different angles
3D wave profile for elliptic source
The ridge near the source of Eathquake
Fronts at different times
The set of profiles
Simulations for Tyrrhenian Sea Relief data: National Oceanic and Atmospheric Administration (NOAA) National Geophysical Data Center (NGDC) ETOPO2 2-minute Global Relief
Rays for imaginary source at Stromboli: 38.8 N, 15.2 E
Amplitudes of wave at different points of the coast
3D wave profile
Density plot
DD7-29/05/07-01/06/07 Special session on tsunami and typhoons Scattering of tsunami on the beach S.Dobrokhotov Inst. Probl. of Mechanics R. Ac Sc. Moscow Petya Zhevandrov Escuela de Ciencias Fisico-Matematicas, Morelia, Mexico Brunello Tirozzi Department of Physics, Univ. “La Sapienza”, Rome
... Workshop on Extreme Events... Max Planck Institut for Complex System Dresden, 30 October-2 November 2006 Analysis of the tsunami event in Algeria 2003 B. Tirozzi (1),F. Raicich (2) (1) Department of Physics, University “La Sapienza”, Rome, Italy (2) CNR, Institute of Marine Sciences, Trieste, Italy
Valencia Barcelona Ibiza Earthquake data (USGS): t0: 18:44:19 GMT, 21 may 2003 USGS: epicenter 36.96°N, 3.63°E, M=6.9, hf=12 km Borerro: epicenter 36.90°N, 3.71°E, M=6.8, hf=10 km, strike=56°
Ellipsoidal deformation M = 6.9 h f = 12 km (Pelinovsky et al., 2001) a = 34 km b = 12 km b 56° a Coordinates: model gridpoints
(Dobrokhotov et al., 2006) a 1 = km -1 Gaussian*cosine deformation = 0 a 2 = km -1 b 1 = km -2 b 2 = km -2 = 56° Coordinates: model gridpoints
Linear theory of the scattering of localized waves on a beach of constant slope S. Dobrokhotov, Petya Zhevandrov, Brunello Tirozzi
Shape of perturbation
Amplitude of the waves at tsunami front
Average of the too fast oscillating WKB solution
Example: beach of costant slope
Momentum equation
Singular Lagrangian manifold
Dynamic on the lagrangian manifold
Dynamic on the phase space
Solutions before and after the scattering of the beach (1/2)
Solutions before and after the scattering of the beach (2/2)
Graphics 1
Graphics 2
Graphics 3
End