Ionospheric–Thermospheric Responses to Geomagnetic Storms from Multi-Instrument Space Weather Data

Author:

Shahzad Rasim1,Shah Munawar1ORCID,Tariq M. Arslan234ORCID,Calabia Andres5ORCID,Melgarejo-Morales Angela6ORCID,Jamjareegulgarn Punyawi7ORCID,Liu Libo248ORCID

Affiliation:

1. Department of Space Sciences, GNSS and Space Education Lab, National Center of GIS and Space Application, Institute of Space Technology, Islamabad 44000, Pakistan

2. Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100045, China

3. Centre for Earthquake Studies, National Centre for Physics, Islamabad 44000, Pakistan

4. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

5. Department of Physics and Mathematics, University of Alcalá de Henares, 28031 Madrid, Spain

6. SCiESMEX, LANCE, Instituto de Geofísica, Unidad Michoacán, Universidad Nacional Autónoma de México, Morelia C.P. 58089, Michoacán, Mexico

7. King Mongkut’s Institute of Technology Ladkrabang, Prince of Chumphon Campus, Chumphon 86160, Thailand

8. Heilongjiang Mohe Observatory of Geophysics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100045, China

Abstract

We analyze vertical total electron content (vTEC) variations from the Global Navigation Satellite System (GNSS) at different latitudes in different continents of the world during the geomagnetic storms of June 2015, August 2018, and November 2021. The resulting ionospheric perturbations at the low and mid-latitudes are investigated in terms of the prompt penetration electric field (PPEF), the equatorial electrojet (EEJ), and the magnetic H component from INTERMAGNET stations near the equator. East and Southeast Asia, Russia, and Oceania exhibited positive vTEC disturbances, while South American stations showed negative vTEC disturbances during all the storms. We also analyzed the vTEC from the Swarm satellites and found similar results to the retrieved vTEC data during the June 2015 and August 2018 storms. Moreover, we observed that ionospheric plasma tended to increase rapidly during the local afternoon in the main phase of the storms and has the opposite behavior at nighttime. The equatorial ionization anomaly (EIA) crest expansion to higher latitudes is driven by PPEF during daytime at the main and recovery phases of the storms. The magnetic H component exhibits longitudinal behavior along with the EEJ enhancement near the magnetic equator.

Funder

National Natural Science Foundation of China

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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