Laboratory study of temporal and spatial evolution of waves excited on water surface initially at rest by impulsive wind forcing

Lev Shemer
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引用次数: 3

Abstract

Evolution of waves excited by wind that varies in time is not yet understood sufficiently well. In the present study, waves generated from rest by an effectively impulsive wind forcing are studied in a small laboratory wind-wave tank. Multiple parameters characterizing evolution of the wave field in time as well as in space are presented. Measurements of the variation with time of the instantaneous surface elevation were performed simultaneously with determination of two components of the instantaneous surface slope at a number of fetches along the test section. For each wind forcing conditions, numerous independent realizations were recorded. Thus, sufficient data were collected for computation of statistically reliable ensemble-averaged values of parameters characterizing the evolving random wind-wave field as a function of time elapsed since the initiation of wind. In each realization, data acquisition started when the water surface was calm, and lasted until statistically steady random wave field conditions were attained. The analysis of the ensemble-averaged wind-wave characteristics indicated that distinct stages in the wind-waves evolution could be identified. These stages were compared with the predictions based on the viscous instability theory and on the random resonant wind-waves generation model.

在脉动风的作用下,初始静止时水面上波浪时空演化的室内研究
受风激发的波浪随时间变化的演变还没有得到充分的了解。在本研究中,在一个小型的实验室风浪箱中,研究了有效的脉冲风强迫在静止时产生的波浪。给出了表征波场在时间和空间上演化的多个参数。测量瞬时地表高程随时间的变化,同时测定沿着测试段的多个取点的瞬时地表坡度的两个分量。对于每个风强迫条件,记录了许多独立的实现。因此,收集了足够的数据,用于计算统计上可靠的随机风浪场演化参数的集合平均值,这些参数是风起后随时间流逝的函数。在每一次实现中,数据采集都是在水面平静时开始的,一直持续到达到统计稳定的随机波场条件。对集合平均风浪特征的分析表明,风浪的演化可以区分出不同的阶段。将这些阶段与基于粘性失稳理论和随机共振风浪产生模型的预测结果进行了比较。
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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