EGU26-17020, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-17020
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Thursday, 07 May, 09:15–09:25 (CEST)
 
Room 1.15/16
Total electron content variations related to seismo-ionospheric precursors and seismic/tsunami waves triggered by the 29 July 2025 Mw 8.8 Kamchatka Earthquake
Jann-Yenq Liu1,2,3, Yun-Cheng Wen2, Fu-Yuan Chang1, Tsung-Yu Wu1, Yuh-Ing Chen1, Rui Song4, Katsumi Hattori5, Chun-Yen Huang6, and Kenji Satake7
Jann-Yenq Liu et al.
  • 1National Central University, Center for Astronautical Physics and Engineering, Taoyuan, Taiwan (jyliu@jupiter.ss.ncu.edu.tw)
  • 2Department of Space Science and Engineering, National Central University, Taoyuan, Taiwan
  • 3Center for Space and Remote Sensing Research, National Central University
  • 4Research Institute of Disaster Medicine, Chiba University, Chiba, Japan
  • 5Center for Environmental Remote Sensing, Chiba University, Chiba, Japan
  • 6Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan
  • 7Department of Earth Sciences, National Central University, Taoyuan, Taiwan

The total electron content (TEC) of the global ionosphere map (GIM) is used to study seismo-ionospheric precursors (SIPs) of the 29 July 2025 Mw 8.8 Kamchatka earthquake. Statistical analyses show that SIPs of GIM TEC significantly frequently decrease specifically over the epicenter area on day 21-26 and 1 before the earthquake.  The distance between northern and southern crests of equatorial ionization anomaly in GIM TEC as well as downward ion velocities measured by advanced ionospheric probe (AIP) onboard FORMOSAT-5 (F5) satellite are used to estimate electric fields associated with the observed SIPs. Results show that the seismo-electric fields related the two SIPs estimated by the GIM TEC and F5/AIP ion velocity are about 1 mV/m westward.  Meanwhile, TEC derived by more than 1,400 ground-based GNSS receiving stations in Japan and Taiwan is employed to examine the spatiotemporal evolution of seismic- and tsunami-traveling ionospheric disturbances (STIDs and TTIDs). A normalized process applied to GNSS TEC clearly shows STIDs and TTIDs traveling with the horizontal speeds of 3.6 km/s and 273.2-215.4 m/s, respectively.  The estimated TTID source is located within about 90 km of the center of the main slip area.

How to cite: Liu, J.-Y., Wen, Y.-C., Chang, F.-Y., Wu, T.-Y., Chen, Y.-I., Song, R., Hattori, K., Huang, C.-Y., and Satake, K.: Total electron content variations related to seismo-ionospheric precursors and seismic/tsunami waves triggered by the 29 July 2025 Mw 8.8 Kamchatka Earthquake, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-17020, https://doi.org/10.5194/egusphere-egu26-17020, 2026.