内冲浪区和斜冲区随机波浪条件下的跨岸流体力学大涡模拟

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Benjamin Tsai, Tian-Jian Hsu, Seok-Bong Lee, Maria Pontiki, Jack A. Puleo, Meagan E. Wengrove
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引用次数: 0

摘要

采用三维大涡模拟与自由表面跟踪方案相结合的方法,模拟了在大浪水槽实验中观测到的跨岸流体力学。主要目的是加深对波浪后冲相互作用及其对观测到的形态动力学影响的理解。模拟了两个案例,以阐明在模拟风暴的早期阶段,波浪后冲水相互作用在护堤侵蚀和沙洲形成这两个不同阶段的关键过程。两种情况的主要区别在于水深:一种情况是有护堤而无沙洲(情况 I),另一种情况是有沙洲而无护堤(情况 II),水深相似。模拟结果与测量数据在自由表面高程、波谱和流速方面的良好一致性(总体威尔莫特一致性指数大于 0.8)验证了模型的技能。研究结果表明,以希尔兹参数为代表的底部剪应力在两种情况下都很重要,可能会造成大量沉积物的迁移。值得注意的是,在没有沙洲的情况下,波浪与后冲的强烈相互作用更为频繁。这些强烈的波浪后冲相互作用导致了明显的水平压力梯度,并通过较高的斯莱思参数加以量化,超过了床面瞬时坍塌的标准。此外,在没有沙洲的情况下,还观察到了更强烈的湍流-河床相互作用,其特点是近河床湍流动能,可能会增加沉积物的悬浮。这些见解对于理解护堤侵蚀的基本机制以及沙洲的形成如何保护海滩进一步受到侵蚀至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Large Eddy Simulation of Cross-Shore Hydrodynamics Under Random Waves in the Inner Surf and Swash Zones

Large Eddy Simulation of Cross-Shore Hydrodynamics Under Random Waves in the Inner Surf and Swash Zones

A 3D large eddy simulation coupled with a free surface tracking scheme was used to simulate cross-shore hydrodynamics as observed in a large wave flume experiment. The primary objective was to enhance the understanding of wave-backwash interactions and the implications for observed morphodynamics. Two simulation cases were carried out to elucidate key processes of wave-backwash interactions across two distinct stages: berm erosion and sandbar formation, during the early portion of a modeled storm. The major difference between the two cases was the bathymetry: one featuring a berm without a sandbar (Case I), and the other, featuring a sandbar without a berm (Case II) at similar water depth. Good agreement (overall Willmott's index of agreement greater than 0.8) between simulations and measured data in free surface elevation, wave spectrum, and flow velocities validated the model skill. The findings indicated that the bottom shear stress, represented by the Shields parameter, was significant in both cases, potentially contributing substantial sediment transport. Notably, the occurrence of intense wave-backwash interactions were more frequent in the absence of a sandbar. These intense wave-backwash interactions resulted in a pronounced horizontal pressure gradient, quantified by high Sleath parameters, exceeding the criteria for momentary bed failure. Additionally, a more vigorous turbulence-bed interaction, characterized by near-bed turbulent kinetic energy, was observed in the case lacking a sandbar, potentially augmenting sediment suspension. These insights are pivotal in understanding the mechanisms underlying berm erosion and how sandbar formation serves to protect further beach erosion.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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