Probabilistic characteristics of narrow-band long-wave run-up onshore

<p>The run-up of random long-wave ensemble (swell, storm surge, and tsunami) on the constant-slope beach is studied in the framework of the nonlinear shallow-water theory in the approximation of non-breaking waves. If the incident wave approaches the shore from the deepest water, run-up charac...

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Main Authors: S. Gurbatov, E. Pelinovsky
Format: Article
Language:English
Published: Copernicus Publications 2019-09-01
Series:Natural Hazards and Earth System Sciences
Online Access:https://www.nat-hazards-earth-syst-sci.net/19/1925/2019/nhess-19-1925-2019.pdf
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spelling doaj-4a2a99ced0c44954a838458b9a7d0c462020-11-25T00:50:11ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812019-09-01191925193510.5194/nhess-19-1925-2019Probabilistic characteristics of narrow-band long-wave run-up onshoreS. Gurbatov0E. Pelinovsky1E. Pelinovsky2National Research University, Lobachevsky State University, Nizhny Novgorod, RussiaNational Research University, Higher School of Economics, Moscow, RussiaInstitute of Applied Physics, Russian Academy of Sciences, Nizhny Novgorod, Russia<p>The run-up of random long-wave ensemble (swell, storm surge, and tsunami) on the constant-slope beach is studied in the framework of the nonlinear shallow-water theory in the approximation of non-breaking waves. If the incident wave approaches the shore from the deepest water, run-up characteristics can be found in two stages: in the first stage, linear equations are solved and the wave characteristics at the fixed (undisturbed) shoreline are found, and in the second stage the nonlinear dynamics of the moving shoreline is studied by means of the Riemann (nonlinear) transformation of linear solutions. In this paper, detailed results are obtained for quasi-harmonic (narrow-band) waves with random amplitude and phase. It is shown that the probabilistic characteristics of the run-up extremes can be found from the linear theory, while the same ones of the moving shoreline are from the nonlinear theory. The role of wave-breaking due to large-amplitude outliers is discussed, so that it becomes necessary to consider wave ensembles with non-Gaussian statistics within the framework of the analytical theory of non-breaking waves. The basic formulas for calculating the probabilistic characteristics of the moving shoreline and its velocity through the incident wave characteristics are given. They can be used for estimates of the flooding zone characteristics in marine natural hazards.</p>https://www.nat-hazards-earth-syst-sci.net/19/1925/2019/nhess-19-1925-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Gurbatov
E. Pelinovsky
E. Pelinovsky
spellingShingle S. Gurbatov
E. Pelinovsky
E. Pelinovsky
Probabilistic characteristics of narrow-band long-wave run-up onshore
Natural Hazards and Earth System Sciences
author_facet S. Gurbatov
E. Pelinovsky
E. Pelinovsky
author_sort S. Gurbatov
title Probabilistic characteristics of narrow-band long-wave run-up onshore
title_short Probabilistic characteristics of narrow-band long-wave run-up onshore
title_full Probabilistic characteristics of narrow-band long-wave run-up onshore
title_fullStr Probabilistic characteristics of narrow-band long-wave run-up onshore
title_full_unstemmed Probabilistic characteristics of narrow-band long-wave run-up onshore
title_sort probabilistic characteristics of narrow-band long-wave run-up onshore
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2019-09-01
description <p>The run-up of random long-wave ensemble (swell, storm surge, and tsunami) on the constant-slope beach is studied in the framework of the nonlinear shallow-water theory in the approximation of non-breaking waves. If the incident wave approaches the shore from the deepest water, run-up characteristics can be found in two stages: in the first stage, linear equations are solved and the wave characteristics at the fixed (undisturbed) shoreline are found, and in the second stage the nonlinear dynamics of the moving shoreline is studied by means of the Riemann (nonlinear) transformation of linear solutions. In this paper, detailed results are obtained for quasi-harmonic (narrow-band) waves with random amplitude and phase. It is shown that the probabilistic characteristics of the run-up extremes can be found from the linear theory, while the same ones of the moving shoreline are from the nonlinear theory. The role of wave-breaking due to large-amplitude outliers is discussed, so that it becomes necessary to consider wave ensembles with non-Gaussian statistics within the framework of the analytical theory of non-breaking waves. The basic formulas for calculating the probabilistic characteristics of the moving shoreline and its velocity through the incident wave characteristics are given. They can be used for estimates of the flooding zone characteristics in marine natural hazards.</p>
url https://www.nat-hazards-earth-syst-sci.net/19/1925/2019/nhess-19-1925-2019.pdf
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