热带海洋学报

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关于一次中烈磁暴中的海洋磁测影响因素分析

涂君, 徐行
  

  1. 中国地质调查局广州海洋地质调查局, 广东 广州 511458


  • 收稿日期:2025-08-28 修回日期:2025-11-16 接受日期:2025-11-24
  • 通讯作者: 徐行
  • 基金资助:

    国家自然科学基金项目(42276086,92158202)

Analysis of factors influencing marine magnetometry on a moderately intense magnetic storm

TU Jun, XU Xing    

  1. Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 511458, China


  • Received:2025-08-28 Revised:2025-11-16 Accepted:2025-11-24
  • Contact: Xu, xing
  • Supported by:

    National Natural Science Foundation of China (42276086,92158202)

摘要: 磁暴或磁扰会干扰海洋磁测,导致所采集资料的质量下降。能否改善磁暴或磁扰对海洋磁测结果影响的程度,这个议题备受学界关注。本文以2024年3月24日至25日西太平洋海洋磁测中受磁暴干扰的案例为分析对象。通过收集、整理与磁暴同时段的地磁台网信息,了解当时地磁场状态。基于此,再对比分析磁暴期间与事后重复测量的海洋磁测原始资料及预处理结果,进而探讨磁测资料受磁暴影响的主要因素及降低其影响的可行性。研究表明,用传统海洋磁测资料处理方法是难以消除磁暴对测量结果的影响,原因在于记录地磁日变校正信息的观测仪器技术性能不足,无法提供高质量、完整的磁暴过程记录,从而降低了海洋磁测数据后处理手段的有效性。然而,通过技术创新,可弥补观测仪器的技术缺陷;结合磁暴过程中的地磁场特征动态信息,并利用AI技术来优化海洋磁测数据的预处理流程,有效减少磁暴对海洋磁测结果的影响是可行的。

关键词: 磁暴, Kp指数, 海洋磁测, 影响因素, 地磁观测台站

Abstract: Magnetic storms or magnetic disturbances can interfere with marine magnetic surveys, resulting in a degradation of the quality of information collected. The topic of whether it is possible to reduce the impact of magnetic storms or magnetic disturbances on the marine magnetic survey results is of great interest to the academic community. In this paper, a case study of marine magnetic surveying disturbed by a magnetic storm on 24-25 March 2024 in the western Pacific Ocean was analysed. We collected and collated information from geomagnetic stations contemporaneous with the magnetic storm to understand the state of geomagnetic field at that time. Based on this, we compared and analysed the raw data and pre-processing results of marine magnetic survey data during magnetic storms and repeated measurements after the storms, and then explored the main factors affecting magnetic survey data by magnetic storms and the feasibility of reducing their effects. The studies have shown that it is difficult to eliminate the influence of magnetic storms on the results of measurements using traditional methods of processing marine magnetic survey data. The reason for this is that the technical performance of observation instruments for recording information on geomagnetic diurnal variations, which cannot provide a high-quality and complete record of magnetic storm processes, reduces the effectiveness of post-processing methods for marine magnetic survey data. However, the technical shortcomings of observation instruments can be remedied through technological innovation. Combining the dynamic information of geomagnetic field features during magnetic storms and using AI technology to optimise the pre-processing process of marine magnetic survey data, it is feasible to effectively reduce the impact of magnetic storms on marine magnetic survey data.

Key words: magnetic storms, Kp index, marine magnetometry, influencing factors, geomagnetic observatories