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Titlebook: Extreme Ocean Waves; Efim Pelinovsky,Christian Kharif Book 20081st edition Springer Science+Business Media B.V. 2008 Ocean.Oceanography.fl

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發(fā)表于 2025-3-21 19:45:11 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Extreme Ocean Waves
編輯Efim Pelinovsky,Christian Kharif
視頻videohttp://file.papertrans.cn/321/320038/320038.mp4
概述Uses fully nonlinear hydrodynamic numerical models to discuss rogue waves.Presents statistics data, analysis of the wave groups and the role of different factors like resonance in the formation and dy
圖書封面Titlebook: Extreme Ocean Waves;  Efim Pelinovsky,Christian Kharif Book 20081st edition Springer Science+Business Media B.V. 2008 Ocean.Oceanography.fl
描述.Extreme, freak or rogue waves are produced by a number of physical mechanisms that focus the water-wave energy into a small area, due to wave instability, chaotic behaviour, dispersion (frequency modulation), refraction (presence of variable currents or bottom topography), soliton interactions, etc. ..During the past thirty years a number of physical models of the rogue wave phenomenon have been intensively developed. Numerous experimental, statistical and theoretical investigations are intended to understand the physics of the huge wave formation, its relation to the environmental conditions and to provide a freak wave design for engineering purposes. The book details the vast progress that has been achieved in the understanding of the physical mechanisms of rogue wave phenomenon in recent years.?The selected articles address such issues as the formation of freak waves due to modulation instability of nonlinear wave field, physical and statistical properties of rogue wave generation in deep water and in shallow water, various models of nonlinear water waves, special analysis of nonlinear resonances between water waves and the relation between observations and freak wave theories.
出版日期Book 20081st edition
關鍵詞Ocean; Oceanography; fluid mechanics; geophysics; nonlinear physics; physical oceanography; rogue waves
版次1
doihttps://doi.org/10.1007/978-1-4020-8314-3
isbn_softcover978-90-481-7839-1
isbn_ebook978-1-4020-8314-3
copyrightSpringer Science+Business Media B.V. 2008
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沙發(fā)
發(fā)表于 2025-3-21 22:38:12 | 只看該作者
Non-Gaussian Properties of Shallow Water Waves in Crossing Seas,ing wave trains generates steep and high amplitude peaks, thus enhancing the deviation of the surface elevation from the Gaussian statistics. The analysis of the skewness and the kurtosis shows that the statistical properties depend on the angle between the two wave trains.
板凳
發(fā)表于 2025-3-22 04:14:17 | 只看該作者
Runup of Long Irregular Waves on Plane Beach,represents an irregular sea state with Gaussian spectrum. The asymptotic of probability functions in the range of large amplitudes for estimation of freak wave formation in the shore is studied. It is shown that average runup height of waves with wide spectrum is higher than that of waves with narrow spectrum.
地板
發(fā)表于 2025-3-22 08:00:20 | 只看該作者
Symbolic Computation for Nonlinear Wave Resonances,efined by (1) integer solutions of the resonance conditions, and (2) coupling coefficients of the dynamical system on the wave amplitudes. General computation algorithms are presented which can be used for arbitrary 3-wave resonant system. Implementation in Mathematica is given for planetary ocean waves. Short discussion concludes the paper.
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發(fā)表于 2025-3-22 22:36:32 | 只看該作者
https://doi.org/10.1007/978-3-540-77831-8represents an irregular sea state with Gaussian spectrum. The asymptotic of probability functions in the range of large amplitudes for estimation of freak wave formation in the shore is studied. It is shown that average runup height of waves with wide spectrum is higher than that of waves with narrow spectrum.
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發(fā)表于 2025-3-23 03:02:32 | 只看該作者
Fuyin Wei,Cyril Alias,Bernd Nocheefined by (1) integer solutions of the resonance conditions, and (2) coupling coefficients of the dynamical system on the wave amplitudes. General computation algorithms are presented which can be used for arbitrary 3-wave resonant system. Implementation in Mathematica is given for planetary ocean waves. Short discussion concludes the paper.
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發(fā)表于 2025-3-23 09:15:54 | 只看該作者
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