Lessons learned from the 2004 Sumatra-Andaman megathrust rupture
The 2004 Sumatra-Andaman earthquake has been extensively studied because of its great
size and devastating consequences. Large amounts of high-quality seismic, geodetic, and …
size and devastating consequences. Large amounts of high-quality seismic, geodetic, and …
Coseismic slip on shallow décollement megathrusts: Implications for seismic and tsunami hazard
For years, many studies of subduction zones and on-land fold-and-thrust belts have
assumed that the frontal portions of accretionary prisms are too weak to rupture …
assumed that the frontal portions of accretionary prisms are too weak to rupture …
Modeling of the 2011 Japan tsunami: Lessons for near-field forecast
Y Wei, C Chamberlin, VV Titov, L Tang… - Pure and Applied …, 2013 - Springer
Abstract During the devastating 11 March 2011 Japanese tsunami, data from two tsunami
detectors were used to determine the tsunami source within 1.5 h of earthquake origin time …
detectors were used to determine the tsunami source within 1.5 h of earthquake origin time …
Quadtree-adaptive tsunami modelling
S Popinet - Ocean Dynamics, 2011 - Springer
The well-balanced, positivity-preserving scheme of Audusse et al.(SIAM J Sci Comput 25
(6): 2050–2065, 2004), for the solution of the Saint-Venant equations with wetting and …
(6): 2050–2065, 2004), for the solution of the Saint-Venant equations with wetting and …
Importance of horizontal seafloor motion on tsunami height for the 2011 Mw= 9.0 Tohoku-Oki earthquake
It is now clear that the 2011 Tohoku-Oki earthquake ruptured the subduction interface all the
way to the Japan Trench. However, there is significant disagreement about just how much …
way to the Japan Trench. However, there is significant disagreement about just how much …
Comparison of earthquake source models for the 2011 Tohoku event using tsunami simulations and near‐field observations
Selection of the earthquake source used in tsunami models of the 2011 Tohoku event affects
the simulated tsunami waveform across the near field. Different earthquake sources, based …
the simulated tsunami waveform across the near field. Different earthquake sources, based …
Tsunamigenic major and great earthquakes (2004–2013): source processes inverted from seismic, geodetic, and sea-level data
Two of the great events, the 2004 Sumatra-Andaman MW 9.2 and the 2011 Tohoku MW 9.0
earthquakes are, respectively, the third and the fourth largest earthquakes seismologically …
earthquakes are, respectively, the third and the fourth largest earthquakes seismologically …
Insights into tectonic hazards since the 2004 Indian Ocean earthquake and tsunami
In 2004, an earthquake of moment magnitude M w 9.1–9.3 ruptured over 1,500 km of the
Sunda megathrust under the Indian Ocean, producing a devastating tsunami and resulting …
Sunda megathrust under the Indian Ocean, producing a devastating tsunami and resulting …
Geological effects and implications of the 2010 tsunami along the central coast of Chile
Geological effects of the 2010 Chilean tsunami were quantified at five near-field sites along
a 200km segment of coast located between the two zones of predominant fault slip. Field …
a 200km segment of coast located between the two zones of predominant fault slip. Field …
The effect of compliant prisms on subduction zone earthquakes and tsunamis
Earthquakes generate tsunamis by coseismically deforming the seafloor, and that
deformation is largely controlled by the shallow rupture process. Therefore, in order to better …
deformation is largely controlled by the shallow rupture process. Therefore, in order to better …