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Interplay of Resonant and Quasi-Resonant Interaction of the Directional Ocean Waves

机译:定向海浪的共振和准共振相互作用

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Recent experimental study of the evolution of random directional gravity waves in deep water provides new insight into the nature of the spectral evolution of the ocean waves and the relative significance of resonant and quasi -resonant wave interaction. When the directional angle containing half the total energy is broader than -20°, the spectrum evolves following the energy transfer that can be described by the four-wave resonant interaction alone. In contrast, in the case of a directionally confined spectrum, the effect of quasi-resonant wave-wave interaction becomes important, and the wave system becomes unstable. When the temporal change of the spectral shape due to quasi resonance becomes irreversible owing to energetic breaking dissipation, the spectrum rapidly downshifts. Under such extreme conditions, the likelihood of a freak wave is high.
机译:最近对深水中随机方向性重力波的演化进行的实验研究为了解海浪频谱演化的性质以及共振和准共振波相互作用的相对重要性提供了新的见识。当包含一半总能量的方向角的宽度大于-20°时,频谱随能量转移而演化,而能量转移可以仅通过四波共振相互作用来描述。相反,在方向受限的频谱的情况下,准谐振波-波相互作用的影响变得重要,并且波系统变得不稳定。当由于高能的破坏耗散而由于准谐振引起的光谱形状的时间变化变得不可逆时,光谱会迅速下降。在这种极端条件下,出现怪胎的可能性很高。

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  • 来源
    《Journal of Physical Oceanography》 |2009年第9期|2351-2362|共12页
  • 作者单位

    Department of Ocean Technology Policy and Environment, Graduate School of Frontier Sciences, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba 277-8563, Japan;

    Institute of Industrial Science, University of Tokyo, Tokyo, Japan;

    Research Institute for Global Change, JAMSTEC, Yokohama, Kanagawa, Japan;

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