Magnetic measurement discrepancies in the Ionosphere prior to the 2025 Kamchatka Mw 8.8 earthquake

Abstract Magnetic field data from Swarm’s magnetometers were investigated during the 2025 M w 8.8 Kamchatka earthquake. The examination focuses on the spatiotemporal distribution of magnetic data with Flag 8, which indicates discrepancies between the scalar and vector magnetometers. Flag 8 was observed along Swarm satellite orbits near the epicenter prior to the earthquake, initially appearing approximately 16 days before the mainshock and persisting until 9 days after. The results indicate that the spatial distribution of Flag 8 exhibits high density and extensive coverage around the epicentral region, showing a close relationship with the earthquake. Further examination suggests that neither polar geomagnetic activity nor the South Atlantic Anomaly can adequately explain the observed pattern. This implies that the observed Flag 8 is more likely associated with the seismic activity in the Kamchatka Peninsula. This study highlights Flag 8 as a complementary tool for detecting pre-earthquake magnetic anomalous phenomenon and advancing earthquake precursor research.

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Publication Details

Journal
Terrestrial Atmospheric and Oceanic Sciences
Published
2026-04-07
DOI
https://doi.org/10.1007/s44195-026-00129-w
Primary Topic
Earthquake Detection and Analysis
Type
article
Field-Weighted Citation Impact
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article

Magnetic measurement discrepancies in the Ionosphere prior to the 2025 Kamchatka Mw 8.8 earthquake

Shenjia Zhang, Longwei Chen, Yang Li, Yongxin Gao et al.
Terrestrial Atmospheric and Oceanic Sciences
Earthquake Detection and Analysis
article

Magnetic measurement discrepancies in the Ionosphere prior to the 2025 Kamchatka Mw 8.8 earthquake

Shenjia Zhang, Longwei Chen, Yang Li, Yongxin Gao, Chieh-Hung Chen, Liwei Zhou, Tianya Luo, Dan Tao, Hong Liu, Jun Hu, Xuemin Zhang
article en

Abstract

Abstract Magnetic field data from Swarm’s magnetometers were investigated during the 2025 M w 8.8 Kamchatka earthquake. The examination focuses on the spatiotemporal distribution of magnetic data with Flag 8, which indicates discrepancies between the scalar and vector magnetometers. Flag 8 was observed along Swarm satellite orbits near the epicenter prior to the earthquake, initially appearing approximately 16 days before the mainshock and persisting until 9 days after. The results indicate that the spatial distribution of Flag 8 exhibits high density and extensive coverage around the epicentral region, showing a close relationship with the earthquake. Further examination suggests that neither polar geomagnetic activity nor the South Atlantic Anomaly can adequately explain the observed pattern. This implies that the observed Flag 8 is more likely associated with the seismic activity in the Kamchatka Peninsula. This study highlights Flag 8 as a complementary tool for detecting pre-earthquake magnetic anomalous phenomenon and advancing earthquake precursor research.

Terrestrial Atmospheric and Oceanic Sciences
Hefei University of Technology (CN), Chengdu University of Technology (CN), Guilin University of Technology (CN), Guangxi Transportation Research Institute (CN), China Earthquake Administration (CN)
Openalex Percentile: Top 5%
Earthquake Detection and Analysis
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