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THE RELATIVE TROUGH FROUDE NUMBER FOR WAVE BREAKING (LABORATORY EXPERIMENTS)

机译:相对破波数(实验室实验)

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摘要

We herein introduce an internal and dynamic mechanism instead of an external static mechanism to greatly improve our understanding and application of wave breaking in numerical models. Physical experiments were performed to discover the relationship between the relative trough Froude number and the initiation of wave breaking with and without current conditions. Tests were also recorded in two ways: raw measurement data (water surface elevations and particle velocities) and cinematography using a digital video camera. The recorded data was later analyzed to determine when and where the waves break in conditions both with and without an ambient current. The similarities between the hydraulic jump and bores are used as a basis for the theory. Use of 1.36 as the critical relative trough Froude number at breaking is recommended for numerical models. Additional laboratory experiments are recommended for plain beach slopes other than 1:20 used in these experiments and for bar/trough beach profiles to study how the Froude number criteria performs as water depths increase landward of the bar.
机译:本文中,我们引入了内部和动态机制,而不是外部静态机制,以极大地提高我们对数值模型中的波浪破碎的理解和应用。进行了物理实验,以发现在有或没有电流条件下,相对波谷弗洛德数与破波起始之间的关系。还以两种方式记录测试:原始测量数据(水表面高程和颗粒速度)和使用数码摄像机的摄影。以后对记录的数据进行分析,以确定在有或没有环境电流的情况下,何时何地波破裂。液压跳跃和孔之间的相似之处被用作该理论的基础。对于数值模型,建议使用1.36作为临界相对谷弗劳德数。建议针对这些实验中使用的1:20以外的平原海滩坡度以及条形/槽形海滩剖面进行其他实验室实验,以研究弗洛德数准则如何随着水深增加,向着陆倾斜。

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