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Total Electron Content during Recurrent and Quiet Geomagnetic Periods at the Koudougou Station in Burkina Faso

Total Electron Content during Recurrent and Quiet Geomagnetic Periods at the Koudougou Station in Burkina Faso

作     者:Saguedo Sawadogo Doua Allain Gnabahou Tinlé Pahima Frédéric Ouattara Saguedo Sawadogo;Doua Allain Gnabahou;Tinlé Pahima;Frédéric Ouattara

作者机构:Research Laboratory in Energetics and Space Weather (LAREME) University of Norbert ZONGO (UNZ) Koudougou Burkina Faso 

出 版 物:《International Journal of Astronomy and Astrophysics》 (天文学与天体物理学国际期刊(英文))

年 卷 期:2023年第13卷第3期

页      面:259-280页

学科分类:070801[理学-固体地球物理学] 07[理学] 0708[理学-地球物理学] 

主  题:Total Electronic Content Geomagnetic Activity Quiet-Day Activity Recurrent-Day Activity Solar Flu 

摘      要:In this work, the comparative study of total electron content (TEC) between recurrent and quiet geomagnetic periods of solar cycle 24 at Koudougou station with geographical coordinates 12°15 N;- 2°20 E was addressed. This study aims to analyze how geomagnetic variations influence the behavior of TEC in this specific region. The geomagnetic indices Kp and Dst were used to select quiet and recurrent days. Statistical analysis was used to interpret the graphs. The results show that the mean diurnal TEC has a minimum before dawn (around 0500 UT) and reaches a maximum value around 1400 UT, progressively decreasing after sunset. In comparison, the average diurnal TEC on recurrent days is slightly higher than on quiet days, with an average difference of 7 TECU. This difference increases with the level of geomagnetic disturbance, reaching 21 TECU during a moderate storm. The study also reveals significant monthly variations, with March and October showing the highest TEC values for quiet and recurrent days, respectively. Equinox months show the highest mean values, while solstice months show the lowest. Signatures of semi-annual, winter and equatorial ionization anomalies were observed. When analyzing annual variations, it was found that the TEC variation depends significantly on F10.7 solar flux, explaining up to 98% during recurrent geomagnetic activity and 92% during quiet geomagnetic activity.

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