极低频数据中的Pc1地磁脉动自动识别  

Automatic detection model for Pc1 geomagnetic pulsation in Extremely Low Frequency data

作　　者：王锋 袁静[1] 韩冰[2] 罗浩[3] 刘庆杰[1] 丰继林[1] 刘海军[1] 韩莹[1] 汤吉[2] WANG Feng;YUAN Jing;HAN Bing;LUO Hao;LIU QingJie;FENG JiLin;LIU HaiJun;HAN Ying;TANG Ji(Institute of Disaster Prevention,Sanhe Hebei 065421,China;Institute of Geology,China Earthquake Administration,Beijing 100029,China;Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China)

机构地区：[1]防灾科技学院,河北三河065421 [2]中国地震局地质研究所,北京100029 [3]中国科学院地质与地球物理研究所,北京100029

出　　处：《地球物理学报》2024年第10期3655-3669,共15页Chinese Journal of Geophysics

基　　金：中国地震局教师科研基金项目(20150109);国家自然科学基金青年基金项目(42104159);河北省教育厅科学研究项目(ZC2023108)资助。

摘　　要：极低频电磁台网成功观测到大量的Pc1地磁脉动事件,研究极低频Pc1地磁脉动的自动识别方法对于全面分析地球空间电磁物理环境具有重要意义.本文采用了YOLOv8目标检测网络、ResNet残差网络和定向特征增强技术,提出了一种基于计算机视觉的Pc1地磁脉动自动识别模型(Automatic Detection Model for Pc1 Geomagnetic Pulsation,简称ADM-Pc1).以大连台站和丽江台站的极低频观测数据为例,利用2015—2016年的数据作为训练集进行模型的监督学习,并使用2017—2022年的数据作为测试集对模型性能进行评估.实验结果显示,ADM-Pc1模型的F1-Score值达到了95%,错分率仅为0.9%,虚警率仅为5.8%,漏检率仅为9%,处理1天数据平均耗时是2.72 s,显著优于现有的最优识别模型.这表明,ADM-Pc1模型在识别效果和计算速度方面均能更好地满足实际工程需求.The Extremely Low Frequency (ELF) electromagnetic network has successfully detected numerous Pc1 geomagnetic pulsation events. To facilitate comprehensive analysis of the geospace environment, it is essential to automatically identify Pc1 events from massive observational data. This study proposes an automated detection model named the Automatic Detection Model for Pc1 Geomagnetic Pulsation (ADM-Pc1). The ADM-Pc1 utilizes the YOLOv8 object detection network, ResNet residual network, and directional feature enhancement technology. This study utilized low-frequency observation data from Dalian and Lijiang electromagnetic stations as a case study. Data from 2015 to 2016 was employed as the training set for supervised learning of the model, while data from 2017 to 2022 served as the test set for evaluating the model's performance. The ADM-Pc1 achieved an F1-score of 95%, a misclassification rate of 0.9%, a false alarm rate of 5.8%, a missed detection rate of 9%, and an average processing time of 2.72 seconds per day of data, outperforming most state-of-the-art methods. These results indicate that the ADM-Pc1 model exhibits high accuracy and robustness. Future work will focus on further developing the automatic recognition prototype system for Pc1 geomagnetic pulsations to meet practical engineering requirements.

关 键 词：Pc1地磁脉动 计算机视觉 自动识别 极低频电磁台网 

分 类 号：P353[天文地球—空间物理学]