Analysis of the tsunami event in Algeria 2003

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Presentation transcript:

Analysis of the tsunami event in Algeria 2003 ... Workshop on Extreme Events ... Max Planck Institut for Complex System Dresden, 30 October-2 November 2006 Analysis of the tsunami event in Algeria 2003 S. Dobrokhotov (1), B. Tirozzi (2), P. Zhevandrov (3), F. Raicich (4) (1) Institute for Problems in Mechanics, RAS, Moscow, Russia (2) Department of Physics, University “La Sapienza”, Rome, Italy (3) Escuela de Ciencias Fisico-Matematicas, Morelia, Mich., Mexico (4) CNR, Institute of Marine Sciences, Trieste, Italy

Barcelona Valencia 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°

Euristic formula for the run-up used by Pelinovsky and Ivanov: but no proofs available!

Ellipsoidal deformation hf = 12 km a 56° b (Pelinovsky et al., 2001) a = 34 km b = 12 km Coordinates: model gridpoints

Gaussian*cosine deformation a1= 1.2 10-2 km-1 a2 = 2.7 10-2 km-1 b1 = 0.5 10-2 km-2 b2 = 4.0 10-2 km-2 = 0 = 56° Coordinates: model gridpoints (Dobrokhotov et al., 2006)

Acknowledgements The observed sea-level data for Ibiza are kindly provided by Dr. B. Perez, Puertos del Estado, Madrid, Spain.

Linear theory of the scattering of localized waves on a beach with constant slope.

Example: Scattering of a packet on a beach with constant slope

The asymptotic formulas