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The statistics of wave height and crest elevation during the December 2012 storm in the North Sea

机译:2012年12月北海风暴期间的波高和波峰高的统计

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This paper concerns new field measurements of wave height and crest elevation probability distributions as measured in the North Sea during a storm in December 2012. The water surface elevation was recorded by Saab WaveRadar REX instruments mounted on eight fixed-jacket platforms in addition to a Datawell Directional Waverider buoy. The storm generated an easterly sea state which peaked well in excess of the 100-year wave height for that direction in the region. Furthermore, 19 freak waves occurred during the storm according to the definition as reported by Haver (2000). The present study demonstrates that the significant steepness and spectral bandwidth during the storm remain almost constant. Consequently, there is little change in the commonly applied design wave height and crest elevation probability distributions throughout the storm. Whilst the bulk of the recorded data was in good agreement with the theoretical distributions, it was demonstrated that when the wind speed was larger than 25 m/s, the measured crest elevation lies above the second-order Forristall distribution.
机译:本文涉及在2012年12月的一次暴风雨中在北海测量的波高和波峰高程概率分布的新现场测量。除Datawell外,Saab WaveRadar REX仪器还记录了水面高程,该仪器安装在八个固定夹套平台上定向Waverider浮标。风暴产生了东风海况,该海浪的峰值远远超过该地区该方向的100年波浪高度。此外,根据Haver(2000)报告的定义,在暴风雨期间发生了19次怪胎波。本研究表明,暴风雨期间的陡峭度和频谱带宽几乎保持恒定。因此,整个暴风雨期间常用的设计波高和波峰高程概率分布几乎没有变化。尽管大部分记录数据与理论分布都非常吻合,但事实证明,当风速大于25 m / s时,测得的波峰高度高于二阶Forristall分布。

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