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Experimental Study of the Statistical Properties of Directionally Spread Ocean Waves Measured by Buoys

机译:浮标测量定向展开海浪统计特性的实验研究

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摘要

Wave-following buoys are used to provide measurements of free surface elevation across the oceans. The measurements they produce are widely used to derive wave-averaged parameters such as significant wave height and peak period, alongside wave-by-wave statistics such as crest height distributions. Particularly concerning the measurement of extreme wave crests, these measurements are often perceived to be less accurate. We directly assess this through a side-by-side laboratory comparison of measurements made using Eulerian wave gauges and model wave-following buoys for randomly generated directionally spread irregular waves representative of extreme conditions on deep water. This study builds on the recent work of McAllister and van den Bremer (2019, ), in which buoy measurements of steep directionally spread focused waves groups were considered. Our experiments confirm that the motion of a wave-following buoy should not significantly affect the measured wave crest statistics or spectral parameters and that the discrepancies observed for in situ buoy data are most likely a result of filtering. This filtering occurs when accelerations that are measured by the sensors within a buoy are converted to displacements. We present an approximate means of correcting the resulting measured crest height distributions, which is shown to be effective using our experimental data.
机译:浮标浮标用于在海洋中提供自由表面升高的测量。它们产生的测量被广泛用于推导波平均参数,例如显着的波形高度和峰值周期,以及诸如Crest高度分布的波浪统计。特别是关于极端波峰的测量,这些测量通常被认为是不太准确的。我们通过使用Eulerian波表和模型波浮标进行的测量的并排实验室比较直接评估这一点,用于随机产生的方向扩散的不规则波在深水上的极端条件。本研究建立了最近的McAllister和Van Den Bremer(2019年)的工作,其中考虑了陡峭定向扩展聚焦波组的浮标测量。我们的实验证实,波浪之后的浮标的运动不应显着影响测量的波峰统计或频谱参数,并且对于原位浮标数据观察到的差异很可能是过滤的结果。当由浮标内的传感器测量的加速度转换为位移时,发生该过滤。我们介绍了校正所得的测量的峰值高度分布的近似手段,其示出了使用我们的实验数据有效。

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