Skip to content
DraconiticResearch
Search Sources API
203,234 studies31 sourcesUpdated 22 min ago
Peer-reviewedCC BY 4.0Scientific Reports

Spatial variability of TEC perturbations and ROTI during the 3 october 2024 X9.0 solar flare: a multi-station GNSS analysis

Abstract

This study investigates the spatially heterogeneous low-latitude ionospheric response to the 3 October 2024 X9.0 solar flare using GNSS observations from seven equatorial and low-latitude stations. TEC, quiet-time differential TEC ( Δ TEC ), and ROTI were analyzed under relatively quiet geomagnetic conditions ( Kp=1 –3). The flare peaked at 12:18 UT, and comparison with quiet-time conditions revealed Δ TEC perturbations of approximately 6–14% at several stations, with pronounced spatial differences. YKRO showed the largest positive perturbation at the flare peak, reaching 12.75 TECU (14.21%), whereas MBAR and CUSV exhibited negative perturbations of −10.98 TECU ( −10.77% ) and −6.14 TECU ( −9.29% ), respectively. However, substantial and sometimes larger Δ TEC variations occurred outside the flare interval, indicating that their magnitude alone cannot establish a flare-driven response. ROTI remained generally below 0.04 TECU min −1 during the flare, with stronger irregularity activity occurring predominantly after sunset. The results indicate a measurable and spatially heterogeneous ionospheric response temporally associated with the X9.0 flare, while highlighting the substantial contribution of intrinsic low-latitude variability. These findings emphasize the importance of multi-station observations and quiet-time normalization for robustly assessing solar-flare-associated ionospheric disturbances.

Related

  1. Interhemispheric differences in field-aligned currents, ground magnetic perturbations, and TEC during the geomagnetic storms of May and October 2024
    Sumanjit Chakraborty, Gopi K. Seemala
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsSolar & stellar physicsarXiv
  2. Catalog of Solar Radio Bursts Detected by the LOFAR LV614 Station at the Irbene Observatory during Solar Cycle 25
    Jānis Šteinbergs, Dmitrii Kolotkov, Valery M. Nakariakov +3
    The Astrophysical Journal Supplement SeriesPeer-reviewedCC BY 4.0Full textSolar & stellar physicsCrossref
  3. Catalogue of Solar Radio Bursts Detected by the LOFAR LV614 Station at the Irbene Observatory during Solar Cycle 25
    Jānis Šteinbergs, Dmitrii Kolotkov, Valery M. Nakariakov +3
    arXivPreprintCC BY 4.0Full textSolar & stellar physicsarXiv
  4. Spatial variability of CH4-to-CO conversion pathways in irradiated gas giant atmospheres: implications for chemical relaxation and 1D quench schemes
    Maria Zamyatina, Éric Hébrard, Harry Baskett +5
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsarXiv
  5. Spatial variability of CH4-to-CO conversion pathways in irradiated gas giant atmospheres: implications for chemical relaxation and 1D quench schemes
    Maria Zamyatina, Ãric Hébrard, Harry Baskett +5
    Monthly Notices of the Royal Astronomical SocietyPeer-reviewedCC BY 4.0Full textSolar & stellar physicsCrossref
BibTeX
@article{data2026spatial,
  title = {{Spatial variability of TEC perturbations and ROTI during the 3 october 2024 X9.0 solar flare: a multi-station GNSS analysis}},
  author = {Efrem Amanuel Data and Geto Kassa Setegn and Daniel Okoh},
  journal = {Scientific Reports},
  year = {2026},
  month = oct,
  doi = {10.1038/s41598-026-71943-y},
  url = {https://www.nature.com/articles/s41598-026-71943-y},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Spatial variability of TEC perturbations and ROTI during the 3 october 2024 X9.0 solar flare: a multi-station GNSS analysis
AU  - Efrem Amanuel Data
AU  - Geto Kassa Setegn
AU  - Daniel Okoh
PY  - 2026
DA  - 2026/10/02
JO  - Scientific Reports
DO  - 10.1038/s41598-026-71943-y
UR  - https://www.nature.com/articles/s41598-026-71943-y
AB  - This study investigates the spatially heterogeneous low-latitude ionospheric response to the 3 October 2024 X9.0 solar flare using GNSS observations from seven equatorial and low-latitude stations. TEC, quiet-time differential TEC ( Δ TEC ), and ROTI were analyzed under relatively quiet geomagnetic conditions ( K_p=1 –3). The flare peaked at 12:18 UT, and comparison with quiet-time conditions revealed Δ TEC perturbations of approximately 6–14% at several stations, with pronounced spatial differences. YKRO showed the largest positive perturbation at the flare peak, reaching 12.75 TECU (14.21%), whereas MBAR and CUSV exhibited negative perturbations of −10.98 TECU ( −10.77% ) and −6.14 TECU ( −9.29% ), respectively. However, substantial and sometimes larger Δ TEC variations occurred outside the flare interval, indicating that their magnitude alone cannot establish a flare-driven response. ROTI remained generally below 0.04 TECU min ^−1 during the flare, with stronger irregularity activity occurring predominantly after sunset. The results indicate a measurable and spatially heterogeneous ionospheric response temporally associated with the X9.0 flare, while highlighting the substantial contribution of intrinsic low-latitude variability. These findings emphasize the importance of multi-station observations and quiet-time normalization for robustly assessing solar-flare-associated ionospheric disturbances.
SN  - 2045-2322
ER  -