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Statistics of long-crested extreme waves in single and mixed sea states

机译:单身和混合海区长冠极浪潮统计

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摘要

Most of the studies on extreme waves are focused on the systems with single-peak wave spectra. However, according to the statistics of occurrence, the bimodal spectral system is also frequent in real sea conditions. In order to summarize the statistics of extreme waves, irregular wave trains under single-peak and bimodal spectra for long durations are simulated in this paper, based on a two-dimensional High Order Spectral (HOS) numerical wave tank. A large number of configurations have been tested under unimodal and bimodal spectra. The investigation on the wave trains under single-peak spectrum indicates that although in conditions often referred as deep water (k(p)h pi), the relative water depth has a significant influence on the probabilities of occurrence of extreme waves. A detailed analysis of the combined effect of Benjamin-Feir Index (BFI) and relative water depth is provided. However, the situation is more complex in real sea conditions, which may exhibit multimodal spectra. We focus in this study on long-crested bimodal spectra characterized by the same significant wave height H-s and mean zero-crossing period T-z of the sea states as the single-peak spectrum. The wave conditions under bimodal spectrum present milder extreme wave statistics than those under single-peak spectrum. In addition, mixed ocean systems with equivalent energy distribution (i.e., Sea-Swell Energy Ratio (SSER) is close to 1.0) and larger separation between partitions (i.e., Intermodal Distance (ID) 0.10) are the less prominent to extreme waves appearance. The comparison of the mixed sea states and the corresponding single independent systems demonstrates that the complexity of the underlying physics of a given sea state (for instance the presence of modulational instability or other nonlinear process) cannot be deduced by an analysis limited to the statistical content of the combined sea state. The wave energy being distributed among frequencies plays a major role. Additionally, Gram-Charlier distribution can accurately predict the probability of large waves (1.5 H/H-s 2.0) compared to the MER distribution, but it underestimates the statistics of the wave height distribution when H/H-s is larger than 2.0 for both single-peak and bimodal states.
机译:大多数关于极端波的研究都集中在具有单峰波光谱的系统上。然而,根据发生的统计数据,双峰谱系统也在真正的海洋状况中频繁。为了总结极端波的统计,基于二维高阶光谱(HOS)数值波罐,在本文中仿真了单峰值和长型持续时间的单峰和双峰光谱下的不规则波列。在单峰和双峰光谱下已经测试了大量配置。单峰光谱下波动列车的研究表明,尽管在通常称为深水(K(P)H> PI)的条件下,相对水深对极端波动发生的概率具有显着影响。提供了对本杰明 - Feir指数(BFI)和相对水深的综合作用的详细分析。然而,实际海洋状况中的情况更复杂,这可能表现出多峰光谱。我们专注于这项研究,其具有相同的显着波高的H-S和平均零交叉时段T-Z作为单峰光谱的长冠的双峰光谱。双峰谱下的波条件存在比单峰光谱在单峰谱下的较高的极端波统计。此外,具有等效能量分布的混合海洋系统(即海膨胀能量比(SSER)接近1.0),并且隔板之间的分离较大(即,同型距离(ID)& 0.10)对极端波的突出较小外貌。混合海区和相应的单个独立系统的比较表明,不能通过限于统计含量的分析推导出给定海状态的底层物理学的复杂性(例如,不稳定性或其他非线性过程)合并的海州。在频率之间分布的波能量发挥着重要作用。另外,与MER分布相比,克哈拉姆分布可以准确地预测大波(1.5& 2.0)的概率,但是当H / HS大于2.0时,低估了波高分布的统计数据单峰和双峰状态。

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