Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework

The transformation of a random wave field in shallow water of variable depth is analyzed within the framework of the variable-coefficient Korteweg-de Vries equation. The characteristic wave height varies with depth according to Green's law, and this follows rigorously from the theoretical model...

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Main Authors: A. Sergeeva, E. Pelinovsky, T. Talipova
Format: Article
Language:English
Published: Copernicus Publications 2011-02-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/11/323/2011/nhess-11-323-2011.pdf
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spelling doaj-e916abfc1d5f4046a0a02dea32bf1fa22020-11-24T21:57:38ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812011-02-0111232333010.5194/nhess-11-323-2011Nonlinear random wave field in shallow water: variable Korteweg-de Vries frameworkA. SergeevaE. PelinovskyT. TalipovaThe transformation of a random wave field in shallow water of variable depth is analyzed within the framework of the variable-coefficient Korteweg-de Vries equation. The characteristic wave height varies with depth according to Green's law, and this follows rigorously from the theoretical model. The skewness and kurtosis are computed, and it is shown that they increase when the depth decreases, and simultaneously the wave state deviates from the Gaussian. The probability of large-amplitude (rogue) waves increases within the transition zone. The characteristics of this process depend on the wave steepness, which is characterized in terms of the Ursell parameter. The results obtained show that the number of rogue waves may deviate significantly from the value expected for a flat bottom of a given depth. If the random wave field is represented as a soliton gas, the probabilities of soliton amplitudes increase to a high-amplitude range and the number of large-amplitude (rogue) solitons increases when the water shallows. http://www.nat-hazards-earth-syst-sci.net/11/323/2011/nhess-11-323-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Sergeeva
E. Pelinovsky
T. Talipova
spellingShingle A. Sergeeva
E. Pelinovsky
T. Talipova
Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
Natural Hazards and Earth System Sciences
author_facet A. Sergeeva
E. Pelinovsky
T. Talipova
author_sort A. Sergeeva
title Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
title_short Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
title_full Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
title_fullStr Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
title_full_unstemmed Nonlinear random wave field in shallow water: variable Korteweg-de Vries framework
title_sort nonlinear random wave field in shallow water: variable korteweg-de vries framework
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2011-02-01
description The transformation of a random wave field in shallow water of variable depth is analyzed within the framework of the variable-coefficient Korteweg-de Vries equation. The characteristic wave height varies with depth according to Green's law, and this follows rigorously from the theoretical model. The skewness and kurtosis are computed, and it is shown that they increase when the depth decreases, and simultaneously the wave state deviates from the Gaussian. The probability of large-amplitude (rogue) waves increases within the transition zone. The characteristics of this process depend on the wave steepness, which is characterized in terms of the Ursell parameter. The results obtained show that the number of rogue waves may deviate significantly from the value expected for a flat bottom of a given depth. If the random wave field is represented as a soliton gas, the probabilities of soliton amplitudes increase to a high-amplitude range and the number of large-amplitude (rogue) solitons increases when the water shallows.
url http://www.nat-hazards-earth-syst-sci.net/11/323/2011/nhess-11-323-2011.pdf
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AT epelinovsky nonlinearrandomwavefieldinshallowwatervariablekortewegdevriesframework
AT ttalipova nonlinearrandomwavefieldinshallowwatervariablekortewegdevriesframework
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