Nonlinear Fourier Analysis Algorithm and Models for Water Waves in Terms of Surface Elevation, Amplitude Modulations

A. Osborne
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Abstract

This paper addresses two issues with regard to nonlinear ocean waves. (1) The first issue relates to the often-confused differences between the coordinates used for the measurement and characterization of ocean surface waves: The surface elevation and the complex modulation of a wave field. (2) The second issue relates to the very different kinds of physical wave behavior that occur in shallow and deep water. Both issues come from the known, very different behaviors of deep and shallow water waves. In shallow water one often uses the Korteweg-deVries that describes the wave surface elevation in terms of cnoidal waves and solitons. In deep water one uses the nonlinear Schrödinger equation whose solutions correspond to the complex envelope of a wave field that has Stokes wave and breather solutions. Here I make clear the relationships between the two ways of characterizing surface waves. Furthermore, and more importantly, I address the issues of matching the two types of wave behavior as the wave motion passes from deep to shallow water, or vice versa. For wave measurements we normally obtain the surface elevation with a wave staff, resistance gauge or pressure recorder for getting time series. Remote sensing applications relate to the use of lidar, radar or synthetic aperture radar for obtaining space series. The two types of wave behavior can therefore crucially depend on where the instrument is placed on the “ground track” or “field” over which the lidar or radar measurements are made. Thus the matching problem from deep to shallow water is not only important for wave measurements, but also for wave modeling. Modern wave models [Osborne, 2010, 2018, 2019a, 2019b] that maintain the coherent structures of wave dynamics (solitons, Stokes waves, breathers, superbreathers, vortices, etc.) must naturally pass from deep to shallow water where the nature of the nonlinear physics, and the form of the coherent structures, change. I address these issues and more herein. This paper is directed towards the development of methods for the real time measurement of waves by shipboard radar and for wave measurements by airplane and helicopter using lidar and synthetic aperture radar. Wave modeling efforts are also underway.
非线性傅立叶分析算法及水波在表面高程、振幅调制方面的模型
本文讨论了关于非线性海浪的两个问题。(1)第一个问题涉及用于测量和表征海洋表面波的坐标之间经常混淆的差异:表面高程和波场的复杂调制。第二个问题涉及在浅水和深水中发生的非常不同的物理波行为。这两个问题都来自于深水波和浅水波的已知的、非常不同的行为。在浅水中,人们经常使用Korteweg-deVries,用余弦波和孤子来描述波面高度。在深水中,人们使用非线性Schrödinger方程,其解对应于波场的复杂包络线,该包络线具有斯托克斯波和呼吸解。在这里,我澄清了表征表面波的两种方法之间的关系。此外,更重要的是,我解决了波浪运动从深水到浅水或反之亦然时两种类型波浪行为的匹配问题。对于波浪测量,我们通常用波浪杖、电阻计或压力记录仪来获得地表高程,以获得时间序列。遥感应用涉及利用激光雷达、雷达或合成孔径雷达获取空间序列。因此,这两种波的行为在很大程度上取决于仪器在激光雷达或雷达测量的“地面轨迹”或“场地”上的位置。因此,深水与浅水的匹配问题不仅对波浪测量很重要,而且对波浪模拟也很重要。现代波浪模型[Osborne, 2010, 2018, 2019a, 2019b]维持波浪动力学的相干结构(孤子、斯托克斯波、呼吸波、超呼吸波、漩涡等)必须自然地从深水传递到浅水,在那里非线性物理的性质和相干结构的形式发生了变化。我在这里讨论这些问题和更多的问题。本文旨在研究船用雷达实时测波方法,以及飞机和直升机利用激光雷达和合成孔径雷达进行测波的方法。波浪建模工作也在进行中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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