We consider the behaviour of solutions to the nonlinear shallow-water equations which describe wave runup on a plane beach, concentrating on the behaviour at and just behind the moving shoreline. We develop regular series expansions for the hydrodynamic variables behind the shoreline, which are valid for any smooth initial condition for the waveform. We then develop asymptotic descriptions of the shoreline motion under localized initial conditions, in particular a localized Gaussian waveform: we obtain estimates for the maximum runup and drawdown of the wave, for its maximum velocities and the forces it is able to exert on objects in its path, and for the conditions under which such a wave breaks down. We show how these results may be exten...
An analysis of the run-up over different beach profiles is performed to evaluate the influence of th...
Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is...
The run-up of solitary-type pulses propagating at a small angle with respect to the shore normal is ...
We consider the behaviour of solutions to the nonlinear shallow-water equations which describe wave ...
Using the records of free surface fluctuations at several locations during the 2011 Japan Tohoku tsu...
The initial value problem of the nonlinear evolution, shoreline motion and flow velocities of long w...
Transformation of waves on sandy beaches, their breaking, set-up and run-up are the main factors ...
The initial value problem of the linear evolution and runup of long waves on a plane beach is analyz...
The tsunami run-up problem is solved non-linearly under the most general initial conditions, that is...
We solve the nonlinear shallow water-wave equations over a linearly sloping beach as an initial-boun...
10 pages, 7 Figures. Accepted to Physical Review Letters. Other author's papers can be downloaded at...
The equations that describe the classical problem of water waves – inviscid, no surface tension and ...
The purpose of this paper is to propose the quasi-linear theory of tsunami run-up and run-down on a ...
This chapter describes the coastal hydrodynamics of ocean waves on beach. A comprehensive study on m...
The dynamics of shallow-water waves at the surface of an inviscid and incompressible fluid over a ba...
An analysis of the run-up over different beach profiles is performed to evaluate the influence of th...
Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is...
The run-up of solitary-type pulses propagating at a small angle with respect to the shore normal is ...
We consider the behaviour of solutions to the nonlinear shallow-water equations which describe wave ...
Using the records of free surface fluctuations at several locations during the 2011 Japan Tohoku tsu...
The initial value problem of the nonlinear evolution, shoreline motion and flow velocities of long w...
Transformation of waves on sandy beaches, their breaking, set-up and run-up are the main factors ...
The initial value problem of the linear evolution and runup of long waves on a plane beach is analyz...
The tsunami run-up problem is solved non-linearly under the most general initial conditions, that is...
We solve the nonlinear shallow water-wave equations over a linearly sloping beach as an initial-boun...
10 pages, 7 Figures. Accepted to Physical Review Letters. Other author's papers can be downloaded at...
The equations that describe the classical problem of water waves – inviscid, no surface tension and ...
The purpose of this paper is to propose the quasi-linear theory of tsunami run-up and run-down on a ...
This chapter describes the coastal hydrodynamics of ocean waves on beach. A comprehensive study on m...
The dynamics of shallow-water waves at the surface of an inviscid and incompressible fluid over a ba...
An analysis of the run-up over different beach profiles is performed to evaluate the influence of th...
Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is...
The run-up of solitary-type pulses propagating at a small angle with respect to the shore normal is ...