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Nonlinear ocean waves and surface currents: A theoretical investigation.

机译:非线性海浪和地表流:理论研究。

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摘要

This thesis contains two parts. In the first part the nonlinear ocean waves and in the second part Eulerian surface currents are studied.;The action balance equation which describes the evolution of wave variance spectrum plays a central role in modern wave modelling. It gives the statistical description of the time evolution of sea waves, which has many applications. The general expression for the source function, in action balance equation consists of three terms representing input energy from wind, the nonlinear transfer and energy dissipation by white capping. The shape and rate of evolution of wind sea spectrum is controlled by the term of nonlinear transfer. The first part of this study is mainly concerned with the approximate solutions of nonlinear transfer action functions that satisfy a set of first order ordinary differential equations. The JONSWAP spectrum is used as initial conditions to solve this problem. Three analytical methods due to Picard, Bernoulli and Adomian and one numerical integration method using fourth order Runge-Kutta scheme are used to compute the nonlinear transfer action functions. The results obtained from these four methods are compared in graphical forms and we have found excellent agreement among them.;The second part of this study is devoted mainly to the determination of the analytic solutions for the Eulerian currents present in ocean circulation. A variety of solutions that satisfy a required boundary and initial conditions are obtained. A Laplace transform method with convolution integral concept is used as a solution technique. Some solution are graphically illustrated, and physical meaning are described.
机译:本文分为两个部分。在第一部分中,研究了非线性海浪,在第二部分中,研究了欧拉表面海流。;描述波方差谱演化的作用平衡方程在现代波浪建模中起着核心作用。它给出了海浪随时间变化的统计描述,具有许多应用。在动作平衡方程中,源函数的一般表达式由三项组成,分别表示风的输入能量,非线性传递和白上限的能量耗散。风海频谱的形状和演化速率受非线性传递项的控制。本研究的第一部分主要涉及满足一组一阶常微分方程的非线性传递作用函数的近似解。 JONSWAP频谱用作解决此问题的初始条件。使用Picard,Bernoulli和Adomian的三种分析方法以及一种使用四阶Runge-Kutta方案的数值积分方法来计算非线性传递作用函数。从这四种方法获得的结果以图形形式进行了比较,我们发现它们之间具有极好的一致性。;本研究的第二部分主要致力于确定海洋环流中欧拉流的解析解。获得满足所需边界和初始条件的各种解决方案。具有卷积积分概念的拉普拉斯变换方法用作求解技术。以图形方式说明了一些解决方案,并描述了物理意义。

著录项

  • 作者

    Sharma, Swastika.;

  • 作者单位

    Dalhousie University (Canada).;

  • 授予单位 Dalhousie University (Canada).;
  • 学科 Mathematics.;Physical Oceanography.
  • 学位 M.Sc.
  • 年度 2003
  • 页码 95 p.
  • 总页数 95
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 非洲史;
  • 关键词

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