Russian Journal of Earth Sciences Russian Journal of Earth Sciences Russian Journal of Earth Sciences 1681-1208 46664 ОРИГИНАЛЬНЫЕ СТАТЬИ ORIGINAL ARTICLES ОРИГИНАЛЬНЫЕ СТАТЬИ Numerical simulation of the 7 February 1963 tsunami in the Bay of Corinth, Greece Numerical simulation of the 7 February 1963 tsunami in the Bay of Corinth, Greece Lobkovsky L I Lobkovsky L I Mazova R Kh Mazova R Kh Garagash I A Garagash I A Kataeva L Yu Kataeva L Yu P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia ru P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia ru Nizhny Novgorod State Technical University, Nizhniy Novgorod, Russia ru Nizhny Novgorod State Technical University, Nizhniy Novgorod, Russia ru Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia ru Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia ru Nizhny Novgorod State Technical University, Nizhniy Novgorod, Russia ru Nizhny Novgorod State Technical University, Nizhniy Novgorod, Russia ru 8 5 1 12 29 10 2021 https://rjes.ru/en/nauka/article/46664/view

The paper addresses the event that occurred in the Bay of Corinth, Greece, on 7 February 1963. The tsunami was produced by a submarine landslide in the mouth of the local Salmenikos River. The paper presents preliminary numerical results obtained in terms of an elastoplastic model for the surface water waves generated by the landslide and propagated onto the coast. The wave propagation is analyzed as a function of the landslide movement. The inferred results are compared with those obtained in terms of other models.

The paper addresses the event that occurred in the Bay of Corinth, Greece, on 7 February 1963. The tsunami was produced by a submarine landslide in the mouth of the local Salmenikos River. The paper presents preliminary numerical results obtained in terms of an elastoplastic model for the surface water waves generated by the landslide and propagated onto the coast. The wave propagation is analyzed as a function of the landslide movement. The inferred results are compared with those obtained in terms of other models.

 tsunami generation shallow water equations aseismic tsunami sedimentary mass. tsunami generation shallow water equations aseismic tsunami sedimentary mass.

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