Ionospheric Total Electron Content Response to the Intense Geomagnetic Storm of 10th -11th May 2024 over Low, Mid and High Latitude Regions
Wilberforce Muniafu *
Department of Physics, Masinde Muliro University of Science & Technology, Kakamega, Kenya.
Edward Uluma
Department of Physics, Masinde Muliro University of Science & Technology, Kakamega, Kenya.
Solomon Otoo Lomotey
Department of Smart Technologies, University of Environment and Sustainable Development, Somanya, Eastern Region, Ghana.
Kouassi Nguessan
Départemente de Physique, Université Nangui Abrogoua, Abidjan, Côte d’Ivoire.
Fashae Joshua Bankole
Physics Programme, Bowen University, Iwo. Osun State, Nigeria.
Chali Idosa Uga
Department of Space Science, University of Alabama in Huntsville, Alabama, USA and Department of Physics, Jimma University, Jimma, Oromia, Ethiopia.
Boniface Ndinya
Department of Physics, Masinde Muliro University of Science & Technology, Kakamega, Kenya.
George Omondi
Department of Physics and Material Science, Maseno University, Maseno, Kenya.
*Author to whom correspondence should be addressed.
Abstract
In this paper, we investigated the response of ionospheric Total electron content (TEC) to the intense geomagnetic storm of 10th - 11th May 2024 using 6 Global Navigation Satellite System (GNSS) stations: BAKE (Geog. Lat.64.33o N; Geog. Lon. 96.02o W), BELE (Geog. Lat. 1.41o S; Geog. Lon. 48.46o W), MBAR (Geog. Lat. 0.60o S; Geog. Lon. 30.74o E), SUTH (Geog. Lat. 32.38o S; Geog. Lon. 20.81o E), BJFS (Geog. Lat. 39.61o N; Geo. Lon. 115.89o E) and DUND (Geog. Lat. 45.88o S; Geog. Lon.170.60o E) situated over low, mid and high latitude regions. The GPS-TEC data was extracted, processed and used to plot vertical total electron content (VTEC) verses universal time (UT) from 8th to 13th May 2024 for each GNSS receiver station. A contour plot of TEC variation was also plotted for each station from 8th to 13th May 2024. The results showed TEC enhancing significantly at the beginning of the storm, during daytime at the geomagnetic equator, with the exception of MBAR, where TEC increased at night. This was attributed to the effect of prompt penetration of electric field (PPEF). A reduction in TEC was also noted on 11th May 2024, during the recovery phase over all the GNSS receiver stations. This was attributed to the effect of the disturbance dynamo electric field (DDEF) and composition change. The contour plots showed diurnal variation in TEC concentration over each GNSS receiver station. The TEC concentration however reduced during the storm period.
Keywords: Geomagnetic storm, total electron content, prompt penetration electric field, disturbance dynamo electric field, global navigation satellite system