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On wave damping occurring during source-based generation of steep waves in deep and near-shallow water

机译:关于在深水和近浅水中基于源的陡波生成过程中发生的波衰减

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Generation of steep waves (H/lambda > 0.03) in a NSE-based NWT is a challenging task and is seldom attempted in near-shallow water (kh < 1.0). Failure towards attainment of the target steepness is characterized by an under prediction of the wave height (H) along the length of the NWT. The issue of height damping has received limited attention in literature. In this context, a NSE based NWT has been developed using a PLIC-VOF formulation and a mass source-based wave generator. Wave damping at the NWT boundaries has been achieved using sponge layers. A total of nine wave designs have been simulated in three categories each of steepness (low, moderate and large) and relative depth (near-shallow, intermediate and deep). Criteria for selecting spatio-temporal resolution within the tank have been determined through parametric analysis. For H/lambda > 0.03, it is seen that wave height reduction in excess of 5% occurs in near-shallow and deep water. It is found that height reduction in deep water is largely attributable to free-surface damping as predicted by Airy theory. However, numerical height damping in near-shallow water is observed to be much stronger, especially near the source. A deeper analysis reveals that mass source-based wave generation induces strong and persistent vortical activity in near-shallow water which in turn leads to dissipation of source-injected momentum. Appropriate modifications in source design, that are aimed at reducing wave-vorticity interactions in the near-field, are proposed for steep wave generation in kh < 1 and kh > 2.5. Substantial improvement in the prediction of far field wave height is hence reported.
机译:在基于NSE的NWT中产生陡波(H / lambda> 0.03)是一项艰巨的任务,很少在近浅水(kh <1.0)中进行尝试。未能达到目标陡度的特征是沿NWT长度的波高(H)预测不足。高度阻尼的问题在文献中很少受到关注。在这种情况下,已经使用PLIC-VOF公式和基于质量源的波发生器开发了基于NSE的NWT。使用海绵层可以实现NWT边界处的波浪阻尼。总共模拟了九种波浪设计,分为三个类别,分别为陡度(低,中和大)和相对深度(近浅,中和深)。通过参数分析确定了在水箱内选择时空分辨率的标准。当H /λ> 0.03时,可以看到在近浅水和深水中波高降低超过5%。如艾里理论所预测的,发现深水高度的降低主要归因于自由表面的阻尼。但是,在近浅水中,数值高度阻尼要强得多,尤其是在水源附近。更深入的分析表明,基于源的大量波浪产生会在近浅水中诱导强烈而持久的涡旋活动,进而导致消散注入源的动量。针对kh <1和kh> 2.5的陡波产生,提出了针对源设计的适当修改,旨在减少近场中的波涡相互作用。因此,据报道,在远场波高的预测上有了实质性的改进。

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