利用电磁数据进行海源估计:全面审查
Toshitaka Baba1, Zhiheng Lin2, Takuto Minami3
1Graduate School of Technology, Industrial and Social Sciences, Tokushima University, Tokushima, Japan.
概括
海底电磁计 (OBEM) 通过测量磁场波动来探测海,显示出有前途的潜力. 虽然面临着噪音挑战,但OBEM提供了独特的速度场观测,补充了传统的压力表.
科学领域:
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
- 电磁主义 电磁主义
背景情况:
- 海底压力表是海监测的标准.
- 最近的研究表明,海期间的磁场波动.
- 海底电磁计 (OBEM) 成为一种潜在的替代技术.
研究的目的:
- 综合有关海磁场的发现及其在源估计中的使用.
- 为了评估OBEMs对海观测的有效性.
- 为了将OBEM与传统压力表进行比较.
主要方法:
- 对海引起的磁场最近的研究进行了审查和综合.
- 对相关频段的OBEM数据特征进行分析.
- 对用于海检测和表征的OBEM和压力表的比较评估.
主要成果:
- 电磁观测显示,有可能检测到小规模海 (厘米尺度).
- 在关键的海频率下,OBEM的背景噪音大约是压力表的10倍.
- 地球的磁场可以干扰海的磁场检测.
结论:
- OBEM 提供了一种对海监测压力表的补充方法.
- OBEM的一个关键优势是它们能够测量海速度场.
- 需要进一步的研究来克服噪音限制,并优化对海观测的OBEM.
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