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Irregular wave runup statistics on plane beaches: application of a Boussinesq-type model incorporating a generating-absorbing sponge layer and second-order wave generation

机译:平面海滩上的不规则波上升统计:结合有吸收波产生的海绵层和二阶波产生的Boussinesq型模型的应用

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摘要

Efficient absorption of reflected waves at the offshore boundary is a prerequisite for the accurate physical or theoretical modelling of long-duration irregular wave runup statistics at uniform, gently sloped beaches. This paper presents an implementation of the method suggested by Zhang et al. (2014) to achieve reflected wave absorption and simultaneous generation and propagation of incident waves in an existing numerical wave flume incorporating a moving boundary wavemaker. A generating–absorbing layer is incorporated within this 1DH hybrid Boussinesq-nonlinear shallow water equation model such that inshore-travelling incident waves, encompassing bound-wave structure approximately correct to second order, propagate unhindered while offshore-travelling reflected waves are absorbed. Once validated, the method is used to compile random wave runup statistics on uniform beach slopes broadly representative of dissipative, intermediate, and reflective beaches. Analyses of the individual runup time series, ensemble statistics and comparison to an empirical formula based on experimental runup data suggest that the main aspects of runup observed in the field are properly represented by the model. Existence of an upper limit on maximum runup is investigated using a simple extreme-value statistical analysis. Spectral saturation is examined by considering ensemble-averaged swash spectra for three representative beach slopes subject to incident waves with two different offshore significant wave heights. All spectra show f^−4 roll-off at high frequencies in agreement with many previous field studies. The effect is also investigated of the swash motions preceding one particular extreme runup event on the eventual maximum runup elevation.
机译:有效地吸收离岸边界处的反射波是在均匀,缓坡海滩上进行长时间不规则波径迹统计的准确物理或理论建模的前提。本文介绍了Zhang等人建议的方法的实现。 (2014年)实现反射波的吸收以及同时合并了移动边界波发生器的现有数值波槽中入射波的同时生成和传播。在此1DH混合Boussinesq-非线性浅水方程模型中并入了一个发电吸收层,这样,在近似于二阶校正的束缚波结构的情况下,近海行进的入射波不受阻碍地传播,而近海行进的反射波被吸收了。一旦得到验证,该方法将用于在均匀代表着耗散海滩,中间海滩和反射海滩的均匀海滩坡度上编制随机波上升统计数据。对单个启动时间序列,集合统计数据以及基于实验启动数据的经验公式进行比较的分析表明,该模型可以适当地表示实地观测到的启动的主要方面。使用简单的极值统计分析来研究最大加速时间上限的存在。通过考虑三个代表性海滩边坡的集合平均斜率频谱来检查光谱饱和度,这些典型海滩边坡具有两个不同的离岸有效波高的入射波。所有频谱均显示f ^ −4在高频下滚降,这与许多先前的现场研究一致。还研究了在一个特定的极端加速事件之前的斜盘运动对最终最大加速高度的影响。

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