Numerical modeling of surface wave development under the action of wind

The numerical modeling of two-dimensional surface wave development under the action of wind is performed. The model is based on three-dimensional equations of potential motion with a free surface written in a surface-following nonorthogonal curvilinear coordinate system in which depth is counted...

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Main Author: D. Chalikov
Format: Article
Language:English
Published: Copernicus Publications 2018-06-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/14/453/2018/os-14-453-2018.pdf
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spelling doaj-8955c9c2257548b880a3f4042f84ac242020-11-25T01:52:01ZengCopernicus PublicationsOcean Science1812-07841812-07922018-06-011445347010.5194/os-14-453-2018Numerical modeling of surface wave development under the action of windD. Chalikov0D. Chalikov1D. Chalikov2Shirshov Institute of Oceanology, Saint Petersburg 199053, RussiaRussian State Hydrometeorological University, Saint Petersburg 195196, RussiaUniversity of Melbourne, Victoria 3010, AustraliaThe numerical modeling of two-dimensional surface wave development under the action of wind is performed. The model is based on three-dimensional equations of potential motion with a free surface written in a surface-following nonorthogonal curvilinear coordinate system in which depth is counted from a moving surface. A three-dimensional Poisson equation for the velocity potential is solved iteratively. A Fourier transform method, a second-order accuracy approximation of vertical derivatives on a stretched vertical grid and fourth-order Runge–Kutta time stepping are used. Both the input energy to waves and dissipation of wave energy are calculated on the basis of earlier developed and validated algorithms. A one-processor version of the model for PC allows us to simulate an evolution of the wave field with thousands of degrees of freedom over thousands of wave periods. A long-time evolution of a two-dimensional wave structure is illustrated by the spectra of wave surface and the input and output of energy.https://www.ocean-sci.net/14/453/2018/os-14-453-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Chalikov
D. Chalikov
D. Chalikov
spellingShingle D. Chalikov
D. Chalikov
D. Chalikov
Numerical modeling of surface wave development under the action of wind
Ocean Science
author_facet D. Chalikov
D. Chalikov
D. Chalikov
author_sort D. Chalikov
title Numerical modeling of surface wave development under the action of wind
title_short Numerical modeling of surface wave development under the action of wind
title_full Numerical modeling of surface wave development under the action of wind
title_fullStr Numerical modeling of surface wave development under the action of wind
title_full_unstemmed Numerical modeling of surface wave development under the action of wind
title_sort numerical modeling of surface wave development under the action of wind
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2018-06-01
description The numerical modeling of two-dimensional surface wave development under the action of wind is performed. The model is based on three-dimensional equations of potential motion with a free surface written in a surface-following nonorthogonal curvilinear coordinate system in which depth is counted from a moving surface. A three-dimensional Poisson equation for the velocity potential is solved iteratively. A Fourier transform method, a second-order accuracy approximation of vertical derivatives on a stretched vertical grid and fourth-order Runge–Kutta time stepping are used. Both the input energy to waves and dissipation of wave energy are calculated on the basis of earlier developed and validated algorithms. A one-processor version of the model for PC allows us to simulate an evolution of the wave field with thousands of degrees of freedom over thousands of wave periods. A long-time evolution of a two-dimensional wave structure is illustrated by the spectra of wave surface and the input and output of energy.
url https://www.ocean-sci.net/14/453/2018/os-14-453-2018.pdf
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