17 pages, 11 figures, 43 references. Other author's papers can be downloaded at http://www.denys-dutykh.com/International audienceThe estimate of individual wave run-up is especially important for tsunami warning and risk assessment as it allows to evaluate the inundation area. Here as a model of tsunami we use the long single wave of positive polarity. The period of such wave is rather long which makes it different from the famous Korteweg-de Vries soliton. This wave nonlinearly deforms during its propagation in the ocean, what results in a steep wave front formation. Situations, when waves approach the coast with a steep front are often observed during large tsunamis, e.g. 2004 Indian Ocean and 2011 15 Tohoku tsunamis. Here we study the n...
Tsunamis are long waves that evolve substantially, through spatial and temporal spreading from their...
The generation of tsunamis with the help of a simple dislocation model of an earthquake and their pr...
Large landslide-tsunamis are caused by mass movements such as landslides or rock falls impacting int...
17 pages, 11 figures, 43 references. Other author's papers can be downloaded at http://www.denys-dut...
International audienceEvaluation of wave run-up characteristics is one of the most important tasks i...
Using the records of free surface fluctuations at several locations during the 2011 Japan Tohoku tsu...
Analytical solutions for the linear and nonlinear shallow-water wave equations are developed for evo...
The process of tsunami evolution during its generation in search for possible amplification mechanis...
A common approach in modeling the generation and propagation of tsunami is based on the assumption o...
Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is...
AbstractAnalytical methods for studying tsunami run-up become untenable when the tsunami wave runs o...
This paper discusses the applications of linear and nonlinear shallow water wave equations in practi...
The various aspects of the propagation of long waves onto a shelf (i.e., reflection, .transmission a...
Tsunamis are long waves that evolve substantially, through spatial and temporal spreading from their...
The generation of tsunamis with the help of a simple dislocation model of an earthquake and their pr...
Large landslide-tsunamis are caused by mass movements such as landslides or rock falls impacting int...
17 pages, 11 figures, 43 references. Other author's papers can be downloaded at http://www.denys-dut...
International audienceEvaluation of wave run-up characteristics is one of the most important tasks i...
Using the records of free surface fluctuations at several locations during the 2011 Japan Tohoku tsu...
Analytical solutions for the linear and nonlinear shallow-water wave equations are developed for evo...
The process of tsunami evolution during its generation in search for possible amplification mechanis...
A common approach in modeling the generation and propagation of tsunami is based on the assumption o...
Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is...
AbstractAnalytical methods for studying tsunami run-up become untenable when the tsunami wave runs o...
This paper discusses the applications of linear and nonlinear shallow water wave equations in practi...
The various aspects of the propagation of long waves onto a shelf (i.e., reflection, .transmission a...
Tsunamis are long waves that evolve substantially, through spatial and temporal spreading from their...
The generation of tsunamis with the help of a simple dislocation model of an earthquake and their pr...
Large landslide-tsunamis are caused by mass movements such as landslides or rock falls impacting int...