Nonlinear long-wave deformation and runup in a basin of varying depth

Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is analyzed in the framework of 1-D nonlinear shallow-water theory. The basin depth is slowly varied far offshore and joins a plane beach near the shore. A small-amplitude linear sinusoidal incident wav...

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Main Author: I. Didenkulova
Format: Article
Language:English
Published: Copernicus Publications 2009-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/16/23/2009/npg-16-23-2009.pdf
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spelling doaj-99c7b78f404a4a488dfcc77c1c477b892020-11-24T23:23:12ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462009-01-011612332Nonlinear long-wave deformation and runup in a basin of varying depthI. DidenkulovaNonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is analyzed in the framework of 1-D nonlinear shallow-water theory. The basin depth is slowly varied far offshore and joins a plane beach near the shore. A small-amplitude linear sinusoidal incident wave is assumed. The wave dynamics far offshore can be described with the use of asymptotic methods based on two parameters: bottom slope and wave amplitude. An analytical solution allows the calculation of increasing wave height, steepness and spectral amplitudes during wave propagation from the initial wave characteristics and bottom profile. Three special types of bottom profile (beach of constant slope, and convex and concave beach profiles) are considered in detail within this approach. The wave runup on a plane beach is described in the framework of the Carrier-Greenspan approach with initial data, which come from wave deformation in a basin of slowly varying depth. The dependence of the maximum runup height and the condition of a wave breaking are analyzed in relation to wave parameters in deep water. http://www.nonlin-processes-geophys.net/16/23/2009/npg-16-23-2009.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. Didenkulova
spellingShingle I. Didenkulova
Nonlinear long-wave deformation and runup in a basin of varying depth
Nonlinear Processes in Geophysics
author_facet I. Didenkulova
author_sort I. Didenkulova
title Nonlinear long-wave deformation and runup in a basin of varying depth
title_short Nonlinear long-wave deformation and runup in a basin of varying depth
title_full Nonlinear long-wave deformation and runup in a basin of varying depth
title_fullStr Nonlinear long-wave deformation and runup in a basin of varying depth
title_full_unstemmed Nonlinear long-wave deformation and runup in a basin of varying depth
title_sort nonlinear long-wave deformation and runup in a basin of varying depth
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2009-01-01
description Nonlinear transformation and runup of long waves of finite amplitude in a basin of variable depth is analyzed in the framework of 1-D nonlinear shallow-water theory. The basin depth is slowly varied far offshore and joins a plane beach near the shore. A small-amplitude linear sinusoidal incident wave is assumed. The wave dynamics far offshore can be described with the use of asymptotic methods based on two parameters: bottom slope and wave amplitude. An analytical solution allows the calculation of increasing wave height, steepness and spectral amplitudes during wave propagation from the initial wave characteristics and bottom profile. Three special types of bottom profile (beach of constant slope, and convex and concave beach profiles) are considered in detail within this approach. The wave runup on a plane beach is described in the framework of the Carrier-Greenspan approach with initial data, which come from wave deformation in a basin of slowly varying depth. The dependence of the maximum runup height and the condition of a wave breaking are analyzed in relation to wave parameters in deep water.
url http://www.nonlin-processes-geophys.net/16/23/2009/npg-16-23-2009.pdf
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