Boussinesq wave models have been introduced in tsunami science with considerable success. Methodical simulations of case studies provide a critical form of validation for these models. In current simulation techniques, developed since the 1998 Papua New Guinea event, carefully derived tsunami sources are input into a fourth order Boussinesq water wave simulation code (Geowave) capable of capturing wave dissipation, wave breaking, wave dispersion, and nonlinear wave activity. When the tsunami source is known, almost all tsunami observations can be captured with a single, direct Boussinesq simulation. Here, we summarize case studies for the following events: 125 k BP, Alika 2, Hawaii, US, 1908 Messina Strait, Italy, 1946 Unimak, Alaska, US, 1...
The Izu-Bonin Mariana (IBM) subduction zone is an over 3000-km long oceanic-oceanic convergence zone...
The March 11, 2011 M9 Tohoku-Oki Earthquake, which is believed to be the largest event recorded in J...
In this study, we considered the accurate calculation of far-field tsunami waveforms by using the sh...
International audienceCase studies of landslide tsunamis require integration of marine geology data ...
International audienceOn 26 November 1999, at 1321 UT, central Vanuatu was struck by a large offshor...
The December 26, 2004 tsunami is one of the most devastating tsunami in recorded history. It was gen...
Abstract—The Papua New Guinea (PNG) tsunami of 1998 is re-examined through a detailed review of the ...
The devastating 26 December 2004 Indian Ocean tsunami stressed the need for assessing tsunami hazard...
A promising tsunami warning system outlined here links Total Electron Content (TEC) disturbances in ...
In the aftermath of the 26 December, 2004 tsunami, several quantitative predictions of inundation fo...
The December 26, 2004 tsunami was perhaps the most devastating tsunami in recorded history, causing ...
In the aftermath of the 26 December, 2004 tsunami, several quantitative predictions of inundation fo...
Abstract Selection of the earthquake source used in tsunami models of the 2011 Tohoku event affects ...
6 Abstract: The December 26, 2004 tsunami was perhaps the most devastating tsunami in recorded histo...
The Izu-Bonin Mariana (IBM) subduction zone is an over 3000-km long oceanic-oceanic convergence zone...
The March 11, 2011 M9 Tohoku-Oki Earthquake, which is believed to be the largest event recorded in J...
In this study, we considered the accurate calculation of far-field tsunami waveforms by using the sh...
International audienceCase studies of landslide tsunamis require integration of marine geology data ...
International audienceOn 26 November 1999, at 1321 UT, central Vanuatu was struck by a large offshor...
The December 26, 2004 tsunami is one of the most devastating tsunami in recorded history. It was gen...
Abstract—The Papua New Guinea (PNG) tsunami of 1998 is re-examined through a detailed review of the ...
The devastating 26 December 2004 Indian Ocean tsunami stressed the need for assessing tsunami hazard...
A promising tsunami warning system outlined here links Total Electron Content (TEC) disturbances in ...
In the aftermath of the 26 December, 2004 tsunami, several quantitative predictions of inundation fo...
The December 26, 2004 tsunami was perhaps the most devastating tsunami in recorded history, causing ...
In the aftermath of the 26 December, 2004 tsunami, several quantitative predictions of inundation fo...
Abstract Selection of the earthquake source used in tsunami models of the 2011 Tohoku event affects ...
6 Abstract: The December 26, 2004 tsunami was perhaps the most devastating tsunami in recorded histo...
The Izu-Bonin Mariana (IBM) subduction zone is an over 3000-km long oceanic-oceanic convergence zone...
The March 11, 2011 M9 Tohoku-Oki Earthquake, which is believed to be the largest event recorded in J...
In this study, we considered the accurate calculation of far-field tsunami waveforms by using the sh...