沿路易斯维尔海底山脉链路从地震声波转换为水下声波
Tiago C A Oliveira1, Dirk Metz1, Ying-Tsong Lin2
1Preparatory Commission for the Comprehensive Nuclear-Test-Ban Treaty Organization, 1400 Vienna, Austria.
The Journal of the Acoustical Society of America
|May 20, 2024
概括
来自大地震的地震波转化为远离震中心的海洋声波. 这项研究发现,这种转换主要发生在路易斯维尔海底山链上,受地震位置和海底山几何学的影响.
科学领域:
- 海洋学 海洋学 海洋学
- 地震学 地震学
- 声学 声学 在声学方面
背景情况:
- 地震到海洋声波的转换是一个复杂的现象.
- 转换位置通常远离地震中心,覆盖数百至数千公里.
研究的目的:
- 为了研究地震到海洋声波转换过程.
- 为了确定这种转换发生的特定位置.
- 分析地质特征对转换的影响.
主要方法:
- 分析来自水音三联站的水音声信号.
- 利用Kermadec弧线 (2014-2022) 沿线发生的15次大地震的数据.
- 使用到达方向和旅行时间计算.
主要成果:
- 地震到声学转换区域主要与路易斯维尔海底山脉链的部分保持一致.
- 转换区的横向范围有很大的差异,大约从300公里到1800公里.
- 转换区的确切位置取决于地震中心和海底山之间的几何关系.
结论:
- 路易斯维尔海链在地震到海洋声波转换过程中发挥着至关重要的作用.
- 了解这种转换对于准确解释地震和水声学数据至关重要.
- 这些发现强调了在波传播研究中考虑水下地质结构的重要性.
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