水动力实验室中海洋极端波浪产生传播过程中的能量分布

IF 3.1 Q2 ENVIRONMENTAL SCIENCES
D. Fadhiliani, M. Ikhwan, M. Ramli, S. Rizal, M. Syafwan
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引用次数: 0

摘要

背景和目的:海洋水动力的不确定性是测试海洋结构作为初始考虑的原因。这种不确定性对地形的自然结构以及海洋栖息地都有影响。在流体力学实验室中,船舶和近海结构用数学模型作为波浪标记的输入进行测试。对于较大的波数,Benjamin Bona Mahony方程在波槽中具有稳定的方向和位置。在其传播过程中,产生的波表现出调制不稳定性和相位奇点现象。这两个因素使本杰明·博纳·马奥尼成为在实验室中产生极端波的有希望的候选人。本研究的目的是研究能量在每次调制频率变化中的分布。用描述相奇点现象的哈密顿公式来观测能量。这些数据对于确定用于产生极端波的参数至关重要。方法:利用本雅明·博纳·马奥尼波群包络线对本雅明·博纳·马奥尼波进行研究。已知Benjamin Bona Mahony波群根据非线性薛定谔方程演化。哈密顿量控制了相位振幅的动态变化,证明了非线性薛定谔方程在有限时间内的奇异性。该哈密顿量由非线性薛定谔的适当拉格朗日量导出,然后转化为位移相幅变量的哈密顿量。结果:在表面水波研究中,势能与波幅有关,动能与波陡有关。时,得到最大波幅和最大陡度。当,由于陡峭,不能形成极端的波浪。这是由于在海岸上有可能将波浪破碎成更小的波浪。在位置上,能量曲线是对称的。结论:根据哈密顿能量分布的描述,调制频率越小,波传播所涉及的势能和动能越大,反之亦然。当调制频率较低时,波的振幅和陡度最大,反之亦然。作为极端波发生器的调制频率是,因为产生的振幅相当高,包络中的能量也相当大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution of energy in propagation for ocean extreme wave generation in hydrodynamics laboratory
BACKGROUND AND OBJECTIVES: The hydrodynamic uncertainty of the ocean is the reason for testing marine structures as an initial consideration. This uncertainty has an impact on the natural structure of the topography as well as marine habitats. In the hydrodynamics laboratory, ships and offshore structures are tested using mathematical models as input to the wave marker. For large wavenumbers, Benjamin Bona Mahony's equation has a stable direction and position in the wave tank. During their propagation, the generated waves exhibit modulation instability and phase singularity phenomena. These two factors refer to Benjamin Bona Mahony as a promising candidate for generating extreme waves in the laboratory. The aim of this research is to investigate the distribution of energy in each modulation frequency change. The Hamiltonian formula that describes the phenomenon of phase singularity is used to observe energy. This data is critical in determining the parameters used to generate extreme waves.METHODS: The envelope of the Benjamin Bona Mahony wave group can be used to study the Benjamin Bona Mahony wave. The Benjamin Bona Mahony wave group is known to evolve according to the Nonlinear Schrodinger equation. The Hamiltonian governs the dynamics of the phase amplitude and proves the Nonlinear Schrodinger equation's singularity for finite time. The Hamiltonian is derived from the appropriate Lagrangian for Nonlinear Schrodinger and then transformed into the Hamiltonian  with the displaced phase-amplitude variable.FINDINGS: Potential energy is related to wave amplitude and kinetic energy is related to wave steepness in the study of surface water waves. When , the maximum wave amplitude and steepness are obtained. When , extreme waves cannot be formed due to steepness. This is due to the possibility of breaking waves into smaller waves on the shore. In terms of position, the energy curve is symmetrical.CONCLUSION: According to Hamiltonian's description of the energy distribution, the smaller the modulation frequency, the greater the potential and kinetic energy involved in wave propagation, and vice versa. While the wave's amplitude and steepness will be greatest for a low modulation frequency, and vice versa. The modulation frequency considered as an extreme wave generator is , because the resulting amplitude is quite high and the energy in the envelope is also quite large.
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来源期刊
CiteScore
7.90
自引率
2.90%
发文量
11
审稿时长
8 weeks
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