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Marine seismic observation of internal solitary wave packets in the northeast South China Sea

机译:南海东北部内部孤立波包的海洋地震观测

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摘要

Recently the novel seismic oceanography method has been reported to be an effective way to study the energetic internal solitary waves (ISWs) in the northern South China Sea. An optimized seismicoceanographic cruise was carried out to observe such near-surface ISWs on Dongsha Plateau in July 2014. Several soliton trains rather than single solitons were captured using the seismic technique. After seismic data processing, one prototypical rank-ordered ISW packet on northeast side of Dongsha Island was clearly identified for further analysis. This included waveforms, propagation velocities, and vertical velocities for individual solitons. In this study, an improved scheme was applied to derive the transient phase velocities from the seismic data which is verified from independent satellite and hydrographic data. Analytical predictions from Korteweg-de Vries equation fit better than the extended Korteweg-de Vries equation ignoring background currents. Our results show that the seismic method can be successfully used to image targets in shallow water below 40 m and that seismic oceanography is a promising technique for studying nearsurface phenomena with high spatial resolution.
机译:最近,据报道,新颖的地震海洋学方法是研究南海北部高能内部孤波(ISW)的有效方法。 2014年7月,进行了优化的地震海洋巡游,以观测东沙高原的近地表ISW。使用地震技术捕获了几列孤子而不是单孤子。经过地震数据处理后,在东沙岛东北侧清楚地识别出一个原型等级排序的ISW数据包,以进行进一步分析。其中包括各个孤子的波形,传播速度和垂直速度。在这项研究中,采用了一种改进的方案来从地震数据中导出瞬态相速度,并通过独立的卫星和水文数据进行了验证。忽略背景电流,通过Korteweg-de Vries方程进行的分析预测比扩展的Korteweg-de Vries方程更适合。我们的结果表明,地震方法可以成功地用于在40 m以下的浅水中成像目标,而地震海洋学是研究具有高空间分辨率的近地表现象的有前途的技术。

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