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Validation of wave breaking in intermediate water wave groups for HOS-NWT with laboratory experiments

机译:实验室实验验证HOS-NWT中间水波群中的波浪分解

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In this paper, a numerical implementation of a eddy viscosity-type wave breaking model in open source HOS-NWT code (Ducrozet et al. 2012) is presented along lines similar to Seiffert & Ducrozet (2018). Due to Eulerian formulations of free surface boundaries in High Order Spectral (HOS) method, wave breaking can't be simulated directly. Hence, detection of onset of wave breaking followed by an appropriate dissipation mechanism needs to be modelled. For this purpose, the aforementioned model is deployed in HOS-NWT. This is followed by a subsequent validation against breaking wave groups generated by second-order corrected focusing signals in intermediate depths under laboratory conditions (Sriram et al. 2015). The mechanism of dissipation is studied against a time-frequency analysis with particular focus on high frequencies that seem to dominate the wave breaking regime.
机译:在本文中,沿着类似于Seiffert&Ducrozet(2018)的线呈现出开源HOS-NWT码中涡粘度型波断裂模型的数值实现(Ducrozet等,2012)。由于高阶光谱(HOS)方法的自由表面边界的欧拉峰配方,不能直接模拟波断裂。因此,需要建模检测波破裂的开始,然后需要进行适当的耗散机制。为此目的,上述模型部署在HOS-NWT中。随后,这是随后对由实验室条件下的中间深度中的二阶校正聚焦信号产生的断开波组的验证(Sriram等,2015)。研究了耗散机制,采用时频分析,特别侧重于似乎主导波破坏方案的高频。

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