Abstract
In this article three main stages of tsunami wave evolution are investigated. At first, the development of disturbances from a given patched elevation of the bottom surface in an incompressible nonviscous fluid of the uniform depth is considered. Then, a tsunami wave diffraction by underwater bottom elevation or cavity is investigated. In this case the shallow water equations are already used, and it is supposed that a cylindrical wave is spread from patched water elevation over the epicentrum. Last, the tsunami propagation and transformation in a shallow water region and its run-up on a beach are investigated on the basis of the improved shallow water theory, taking into consideration the nonlinear and dispersive terms of higher order. The proposed theory is tested in a problem of collisions of two solutions. Solutions of the first and the second problems are obtained by the method of integral Laplace’s transformation with following numerical inversion of transformations. A finite difference method for a solution of the last problem is used.
| Original language | English |
|---|---|
| Pages (from-to) | 149-165 |
| Number of pages | 17 |
| Journal | Marine Geodesy |
| Volume | 6 |
| Issue number | 2 |
| DOIs | |
| State | Published - 1 Jan 1983 |
| Externally published | Yes |
ASJC Scopus subject areas
- Oceanography