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Modeling of the propagation and evolution of nonlinear waves in a wave train

机译:波列中非线性波传播和演化的建模

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摘要

A theoretical approach is applied to predict the propagation and evolution of nonlinear water waves in a wave train. A semi-analytical solution was derived by applying an eigenfunction expansion method. The solution is applied to study the evolution of nonlinear waves in a wave train and the formation of freak waves. The analysis focuses on the changes of wave profile and wave spectrum due to the interaction of wave components in a wave train. The results indicate that for waves of very low steepness, the changes of wave profile and wave spectrum are of secondary importance and weakly nonlinear wave theories can be applied to describe wave propagation in a wave train. For waves of low and moderate steepness, the nonlinear terms in the free-surface boundary conditions are becoming more and more important and weakly nonlinear wave theories cannot be applied to describe substantial changes in wave profile. A train of basically sinusoidal waves may drastically change its form within a relatively short distance from its original position and freak waves are often formed. The interaction between waves in a wave train and significant wave evolution has substantial effects on a wave spectrum. A train of initially very narrow-banded spectrum changes its simple one-peak spectrum to a broad-banded and often multi-peak spectrum in a fairly short period of time. The analysis shows that these phenomena cannot be described properly by the nonlinear Schrodinger equation or its modifications. Laboratory experiments were conducted in a wave flume to verify theoretical approaches. The free-surface elevation recorded by a system of wave gauges was compared with the results provided by the semi-analytical solution. Theoretical results are in a fairly good agreement with experimental data. A reasonable agreement between theoretical results and experimental data is observed, even for complex changes of long wave trains.
机译:应用理论方法来预测非线性水波在波列中的传播和演化。通过应用本征函数展开法得出半解析解。该解决方案用于研究波列中非线性波的演化以及畸形波的形成。分析着重于由于波列中波分量相互作用而引起的波剖面和波谱变化。结果表明,对于陡度非常低的波,波廓和波谱的变化具有次要的重要性,并且可以应用弱非线性波理论来描述波在波列中的传播。对于低和中等陡度的波浪,自由表面边界条件中的非线性项变得越来越重要,并且弱非线性波浪理论不能用于描述波浪形的实质性变化。一串基本为正弦波的波形可能会在距其原始位置相对较短的距离内急剧改变其形式,并且经常会形成畸形波。波列中的波与显着的波演化之间的相互作用对波谱具有重大影响。一列最初非常窄带的频谱会在相当短的时间内将其简单的单峰频谱变为宽谱带且通常为多峰频谱。分析表明,这些现象不能通过非线性Schrodinger方程或其修正形式正确描述。在波浪槽中进行了实验室实验,以验证理论方法。将波谱仪系统记录的自由表面标高与半解析解提供的结果进行了比较。理论结果与实验数据相当吻合。即使对于长波列的复杂变化,也可以观察到理论结果和实验数据之间的合理一致性。

著录项

  • 来源
    《Archives of Mechanics》 |2011年第3期|p.311-335|共25页
  • 作者

    W. SULISZ; M. PAPROTA;

  • 作者单位

    Department of Wave Mechanics and Structural Dynamics Institute of Hydroengineering Polish Academy of Sciences Koscierska 7 80-328 Gdansk, Poland;

    Department of Wave Mechanics and Structural Dynamics Institute of Hydroengineering Polish Academy of Sciences Koscierska 7 80-328 Gdansk, Poland;

  • 收录信息 美国《科学引文索引》(SCI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    nonlinear waves; wave instability; wave evolution; initial conditions;

    机译:非线性波波不稳定波浪演化初始状态;

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