对比和组合匹配的场和模态分散反转在新英格兰泥的海床地球声学配置文件
Stan E Dosso1, Preston S Wilson2, David P Knobles3
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia, V8W 2Y2, Canada.
The Journal of the Acoustical Society of America
|June 4, 2025
概括
匹配场 (MF) 逆转提供了比模态分散 (MD) 逆转更详细的海底地声结构和衰减配置文件. MF反向为声波形状分析提供了优越的信息内容.
科学领域:
- 海洋学 海洋学 海洋学
- 声学 声学 在声学方面
- 地质物理学 地质物理学
背景情况:
- 海底的地声逆转利用了声波形数据.
- 模式分散 (MD) 和匹配场 (MF) 数据处理是关键技术.
- 了解海底的特性对于声学传播至关重要.
研究的目的:
- 为了比较MD和MF数据的信息内容,用于海底地声逆转.
- 为了评估结合MD和MF数据的联合倒置的有效性.
- 评估海底地球声学特性的分辨率,包括衰减.
主要方法:
- 来自2017年海底特性实验记录的声波形式的分析.
- 对MD和MF数据应用跨维贝叶斯反转.
- 海底模型层的概率抽样和自回归误差模型顺序.
主要成果:
- 与MD逆转相比,MF逆转可以解决更细的地球声学结构,不确定性减少.
- 多频逆转成功估计了海底衰减概况在一个广泛的频段 (20-1504 Hz).
- 联合倒置受益于MD和MF数据的互补优势.
结论:
- 匹配场反转提供了优越的地声信息内容,特别是在衰减和详细结构方面.
- 模态分散逆转在更高的频率上面临着挑战.
- 该研究强调了MF反转在全面的海底表征方面的优势.
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