J Behrens, F Dias - … Transactions of the Royal Society A …, 2015 - royalsocietypublishing.org
Tsunamis are rare events with severe consequences. This generates a high demand on accurate simulation results for planning and risk assessment purposes because of the low …
PJ Lynett, K Gately, R Wilson, L Montoya, D Arcas… - Ocean Modelling, 2017 - Elsevier
To help produce accurate and consistent maritime hazard products, the National Tsunami Hazard Mitigation Program organized a benchmarking workshop to evaluate the numerical …
In this study, we considered the accurate calculation of far-field tsunami waveforms by using the shallow water equations and accounting for the effects of Boussinesq dispersion …
Abstract Two hazardous typhoons, Lionrock (August 2016) and Jebi (September 2018), destructively affected the coast of Japan and produced extreme sea level variations. The …
D Melgar, Y Bock - Journal of Geophysical Research: Solid …, 2013 - Wiley Online Library
Computation of tsunami models in the region adjacent to large earthquakes immediately after rupture initiation remains a challenging problem. Limitations of traditional seismological …
PJ Lynett, J Borrero, S Son, R Wilson… - Geophysical Research …, 2014 - Wiley Online Library
The occurrence of tsunami damage is not limited to events causing coastal inundation. Even without flooding, maritime assets are vulnerable to significant damage from strong currents …
The ability to measure, predict, and compute tsunami flow velocities is of importance in risk assessment and hazard mitigation. Substantial damage can be done by high velocity flows …
RI Wilson, AR Admire, JC Borrero, LA Dengler… - Pure and Applied …, 2013 - Springer
The coast of California was significantly impacted by two recent teletsunami events, one originating off the coast of Chile on February 27, 2010 and the other off Japan on March 11 …
Tsunami modeling and simulation has changed in the past few years more than it has in decades, especially with respect to coastal inundation. Among other things, this change is …