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Nonlinear interactions among internal tidal waves in the northeastern South China Sea

机译:南海东北部内部潮汐的非线性相互作用

摘要

We used a set of 75-day long ADCP data from the northeastern South China Sea (SCS) to investigate nonlinear interactions among freely propagating internal tidal waves. The kinetic energy spectra displayed significant peaks at some higher tidal frequencies, such as O1M2 (O-1+M-2), and M-4 (M-2+M-2), where O-1 is the lunar diurnal internal tide, M-2 is the lunar semidiurnal internal tide, and M-4 is the first higher harmonic frequency of M-2. These higher tidal harmonic frequency peaks, as well as the fundamental tidal harmonic peaks, show a sigma (-2.3) spectral falloff rate with frequency. In addition, we explored the possible generation mechanism of higher tidal harmonics. Analysis on the rotary and bicoherence spectra suggests that strong forced non-resonant interaction induced by nonlinear advections was the dominant physical mechanism that induced these higher tidal harmonics. Moreover, the energetic, freely propagating semidiurnal (M-2) internal tidal wave played the most crucial role in these interactions. These results indicate that strong nonlinear forced non-resonant interactions among internal tides can be one of the processes responsible for the redistribution of energy in the internal wave spectrum.
机译:我们使用了一组来自南海东北部(SCS)的75天长的ADCP数据来研究自由传播的内部潮汐波之间的非线性相互作用。动能谱在一些较高的潮汐频率处显示明显的峰值,例如O1M2(O-1 + M-2)和M-4(M-2 + M-2),其中O-1是月日内潮M-2是月球半日内潮,M-4是M-2的第一个高次谐波频率。这些较高的潮汐谐波频率峰值以及基本的潮汐谐波峰值显示出随频率变化的sigma(-2.3)频谱衰减率。此外,我们探索了可能产生更高潮汐谐波的机理。对旋转和双相干谱的分析表明,由非线性对流引起的强强迫非共振相互作用是引起这些较高潮汐谐波的主要物理机制。此外,在这些相互作用中,能量旺盛的,自由传播的半日潮汐(M-2)内部潮汐起着至关重要的作用。这些结果表明内部潮汐之间强烈的非线性强迫非共振相互作用可能是导致内部波谱中能量重新分布的过程之一。

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    Xie XH; Shang XD; Chen GY;

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  • 年度 2010
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