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Article

Strong Longitudinal and Latitudinal Differences of Ionospheric Responses in North American and European Sectors During the 10–11 October 2024 Geomagnetic Storm

1
State Key Laboratory of Solar Activity and Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, China
2
University of Chinese Academy of Sciences, Beijing 100049, China
*
Author to whom correspondence should be addressed.
Remote Sens. 2026, 18(2), 256; https://doi.org/10.3390/rs18020256
Submission received: 11 December 2025 / Revised: 7 January 2026 / Accepted: 12 January 2026 / Published: 13 January 2026

Abstract

This study examines the spatiotemporal evolution of midlatitude ionospheric disturbances during the intense geomagnetic storm on 10–11 October 2024, focusing on the North American and European sectors. It utilizes multi-instrument datasets from ground-based observations, including Global Navigation Satellite System (GNSS) receivers and ionosondes, supplemented by the measurements from the Swarm, DMSP and GUVI/TIMED satellites. The results reveal significant longitudinal and latitudinal variations in regional ionospheric responses, specifically related to Storm Enhanced Density (SED) and the midlatitude trough. Key findings include: (a) During the main phase of the storm, the North American midlatitude ionosphere exhibited a pronounced longitudinal contrast: a positive SED-driven phase in the west versus a negative trough-dominated phase in the east. In the early recovery phase, the western sector transitioned to a trough-induced negative phase, while the eastern sector showed a positive phase related to auroral particle precipitation during substorms. (b) The North American SED featured a strong northwest-extending plume with a westward shift velocity of 200–300 m/s at 45°N, and a sharp density gradient of 60–65 TECU on its northeastern side, in contrast to the trough. (c) The European sector displayed a “sandwich-like” latitudinal pattern, with “positive–negative–positive” variations during the storm. (d) The European sector’s storm-time trough expanded rapidly equatorward, reaching a minimum of ~35° magnetic latitude (MLAT), while broadening latitudinally to a width of 18–20°. These density gradient structures, along with the longitudinal/latitudinal differences, highlight the dynamic processes occurring in the magnetosphere–ionosphere–thermosphere system during intense storms and contribute to the understanding of storm-response mechanisms across different sectors.
Keywords: 10–11 October 2024 geomagnetic storm; longitudinal and latitudinal differences; SED; the midlatitude trough; ionospheric response 10–11 October 2024 geomagnetic storm; longitudinal and latitudinal differences; SED; the midlatitude trough; ionospheric response

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MDPI and ACS Style

Luo, X.; Aa, E.; Wang, X.; Luo, B. Strong Longitudinal and Latitudinal Differences of Ionospheric Responses in North American and European Sectors During the 10–11 October 2024 Geomagnetic Storm. Remote Sens. 2026, 18, 256. https://doi.org/10.3390/rs18020256

AMA Style

Luo X, Aa E, Wang X, Luo B. Strong Longitudinal and Latitudinal Differences of Ionospheric Responses in North American and European Sectors During the 10–11 October 2024 Geomagnetic Storm. Remote Sensing. 2026; 18(2):256. https://doi.org/10.3390/rs18020256

Chicago/Turabian Style

Luo, Xinyue, Ercha Aa, Xin Wang, and Bingxian Luo. 2026. "Strong Longitudinal and Latitudinal Differences of Ionospheric Responses in North American and European Sectors During the 10–11 October 2024 Geomagnetic Storm" Remote Sensing 18, no. 2: 256. https://doi.org/10.3390/rs18020256

APA Style

Luo, X., Aa, E., Wang, X., & Luo, B. (2026). Strong Longitudinal and Latitudinal Differences of Ionospheric Responses in North American and European Sectors During the 10–11 October 2024 Geomagnetic Storm. Remote Sensing, 18(2), 256. https://doi.org/10.3390/rs18020256

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