首页> 外文会议>25th International Conference on Offshore Mechanics and Arctic Engineering 2006(OMAE2006) vol.2: Ocean Engineering; Polar and Arctic Sciences and Technology >A METHOD TO IMPLEMENT THE RANDOM SIGNALS FOR TIME VARYING OFFSHORE WAVE HEIGHT DURING STORM CONDITION IN AN INTRA-WAVE PERIOD WAVE MODEL
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A METHOD TO IMPLEMENT THE RANDOM SIGNALS FOR TIME VARYING OFFSHORE WAVE HEIGHT DURING STORM CONDITION IN AN INTRA-WAVE PERIOD WAVE MODEL

机译:波周期模型中风暴条件下随时间变化离岸波高的随机信号实现方法

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In this paper, a method to implement the surface elevation at the offshore boundary during storm conditions is presented in the intra-wave period wave model. At storm condition, the offshore incident significant wave height is time varying. In the case of time varying incident wave height, the JONSWAP energy spectrum can be manipulated as follows: H_(1/3)~2s(f). s(f) is the energy density function for a unit wave height. During a storm event not only the offshore boundary significant wave heights but also the peak frequency varies. If we choose a mean peak frequency during a storm event, s(f) can be calculated for the mean peak frequency for the storm event. The amplitudes of the component waves for the random signals are calculated from the unit energy density function s(f), and the phase angle of the component wave, So we can numerically generate surface elevation time series for the time varying offshore wave heights. The method was verified in the intra-wave period wave model using field measurements at Sea Palling site Norfolk UK.
机译:本文提出了一种在波内周期波模型中实现暴风雨条件下海上边界地表高程的方法。在风暴条件下,近海事件的重要波高是随时间变化的。在随时间变化的入射波高度的情况下,JONSWAP能谱可以按以下方式操纵:H_(1/3)〜2s(f)。 s(f)是单位波高的能量密度函数。在暴风雨期间,不仅海上边界的重要波高,而且峰值频率也会变化。如果我们选择暴风雨事件期间的平均峰值频率,则可以计算出暴风雨事件的平均峰值频率的s(f)。根据单位能量密度函数s(f)和分量波的相位角,计算出随机信号的分量波的振幅,因此我们可以为随时间变化的海上波浪高度数值生成地表高程时间序列。该方法在海浪周期波模型中使用英国Sea Palling网站的现场测量结果进行了验证。

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