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Alexander B. Rabinovich
Researcher at Shirshov Institute of Oceanology
Publications - 114
Citations - 4812
Alexander B. Rabinovich is an academic researcher from Shirshov Institute of Oceanology. The author has contributed to research in topics: Tide gauge & Meteotsunami. The author has an hindex of 38, co-authored 108 publications receiving 4192 citations. Previous affiliations of Alexander B. Rabinovich include Ocean Institute & Russian Academy of Sciences.
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The Global Reach of the 26 December 2004 Sumatra Tsunami
Vasily V. Titov,Alexander B. Rabinovich,Alexander B. Rabinovich,Harold O. Mofjeld,Richard E. Thomson,Frank I. Gonzalez +5 more
TL;DR: Numerical model simulations, combined with tide-gauge and satellite altimetry data, reveal that wave amplitudes, directionality, and global propagation patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orientation and intensity of the offshore seismic line source and subsequently by the trapping effect of mid-ocean ridge topographic waveguides.
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Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band
Sebastià Monserrat,Sebastià Monserrat,Ivica Vilibić,Alexander B. Rabinovich,Alexander B. Rabinovich +4 more
TL;DR: In this paper, the authors considered tsunami-like waves that are induced by atmospheric processes rather than by seismic sources and provided an overview of meteorological tsunamis in the World Ocean.
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The Grand Banks landslide-generated tsunami of November 18, 1929: preliminary analysis and numerical modeling
TL;DR: In this paper, the authors used a shallow-water model to simulate the slide-generated tsunami from a large submarine slope failure, which was transformed into a turbidity current carrying mud and sand eastward up to 1000 km at estimated speeds of about 60-100 km/h, breaking 12 telegraph cables.
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Spectral analysis of tsunami waves: Separation of source and topography effects
TL;DR: In this paper, a new approach is proposed to separate the influence of source and topography in observed tsunami spectra and to reconstruct the initial source spectrum, assuming a linear tide gauge response to external forcing and is based on comparative analysis of tsunami and background spectra.