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作 者:崔成[1,2] 肖辉[1,2] 左书华[1,2] 张义丰[1,2]
机构地区:[1]交通运输部天津水运工程科学研究所,天津300456 [2]港口水工建筑技术国家工程实验室,天津300456
出 处:《海洋科学进展》2016年第3期377-387,共11页Advances in Marine Science
基 金:国家自然科学基金项目--量化分析三维畸形波内部结构(51509120)
摘 要:采用流体体积(VOF)方法捕捉自由表面,结合有限差分方法求解N-S(Navier-Stokes)方程、k-ε模型封闭,建立数值模型,并使用该模型模拟非平底地形条件下畸形波的生成。采用小波分析方法计算模拟结果的时频能量谱,基于计算结果分析非平底地形对畸形波能量集中程度和高频能量的影响。主要结论为:坡度小于1∶10的斜坡地形和无量纲水深变化小于0.333的曲线地形对畸形波时频能量谱的影响不显著;坡度大于1∶10的斜坡地形和无量纲水深变化大于0.333的曲线地形会显著影响畸形波的时频能量谱,随着坡度和无量纲水深变化的增加,时频能量谱中畸形波发生时刻附近,能量向高频方向移动,使得能量在高频端的分布范围增大,时频谱密度峰值减小;斜坡和曲线地形的特征变化对于畸形波能量集中度参数的影响不显著。A numerical model that solves the Reynolds time-averaged N-S equations by the finite-difference method was built with the k-εmodel for the turbulence closure and the volume of fluid(VOF)method for tracking the free surface.The model was implemented to simulate the freak waves over non-flat bottom topography.With the time-frequency energy spectrum of the freak waves that was calculated by the wavelet analysis method the effects of non-flat bottom topography on the energy focusing and high frequency energy were analyzed.It is concluded that the non-flat bottom topography has a insignificant effect on the timefrequency energy spectrums for the slope that is less than 1∶10and the topography whose normalized change in water depth is smaller than 0.333,but the influence of the non-flat bottom topography is considerable for the slope that is more than 1∶10and the topography whose normalized change in water depth is greater than 0.333.With the increasing slope and normalized change in water depth,the energy shifts to high frequency endwhich makes the frequency domain of the energy distribution broaden,and the peak value of the time-frequency spectrum density decreases.On the other hand,the non-flat bottom topography has a indifferent effect on the parameters of energy focusing.
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