Characterization of Equatorial Electrojet Current in Africa Sector Using Two Approaches

A. O. Idowu *

Department of Physics, University of Ilorin, Kwara, Nigeria.

I. A. Adimula

Department of Physics, University of Ilorin, Kwara, Nigeria.

*Author to whom correspondence should be addressed.


Abstract

Variations in the Equatorial Electrojet (EEJ) ground strength is estimated in three stations (Addis-Ababa - AAB, Ilorin - ILR and Lagos - LAG) in the Africa sector using MAGDAS data collected from September to December, 2008.  Hourly data of the horizontal magnetic field component was used in the study. The EEJ strength was studied using the observed and model simulation approach to determine the correlation and error in their results. The EEJ strength in the stations was estimated with respect to Maputo located off-dip equator. The maximum strength of magnetic effect of the EEJ at the ground level was observed in AAB with a value of 62.98 nT in December, followed by ILR with 57.51 nT in November, and LAG with 46.76 nT in December. The model simulation presented higher values compared to the observed EEJ values with the highest peak variation of 130 nT in AAB (October), 103 nT in ILR (December), and 79.32 nT in LAG (December). Correlation analysis and Root mean square error (RMSE) was carried between the two methods. Lagos (LAG) presented the best correlation and the least RMSE (0.85 and 0.18) in November, while the least suitable fit was noticed in September with RMSE of 8.15 in Addis Ababa (AAB).

Keywords: Equatorial electrojet, dip equator, MAGDAS, fambitakoye model, e-region, solar quiet.


How to Cite

Idowu, A. O., and I. A. Adimula. 2020. “Characterization of Equatorial Electrojet Current in Africa Sector Using Two Approaches”. International Astronomy and Astrophysics Research Journal 2 (1):115-23. https://journaliaarj.com/index.php/IAARJ/article/view/20.

Downloads

Download data is not yet available.

References

Stewart B. Hypothetical views regarding the connection between state of the sun and terrestrial magnetism in “Encyclopedia Brittanica”, 9th edition. 1882;16:181-184.

Chapman S. The equatorial electrojet as detected from the abnormal electric current distribution above Huancayo and elsewhere, Arch.Meteorl. Geophys. Bioclimatol. 1951;4:368-392.

Onwumechili CA. In: Eds. Matsushuita S. and Campbell, W. H. Physics of Geomagnetic Phenomena. Academic press, New York. 1967;1:425-507.

Luhr H, Maus S. Direct observation of the F-region dynamo currents and the spatial structure of the EEJ by CHAMP. Geophys. Res. Lett. 2006;33:24102.

Chandra H, Sinha HSS, Rastogi RG. Equatorial electrojet studies from rocket and ground measurements. Earth Planets Space. 2000;52:111– 120.

Manoj C, Luhr H, Maus S, Nagarajan N. Evidence for short spatial correlation lengths of the noontime equatorial electrojet inferred from a comparison of satellite and ground magnetic data. J. Geophys. Res. 2006;111:11312.

Available:http://dx.doi.org/10.1029/2006JA011855.

Adimula IA, Rabiu AB, Yumoto Y. the MAGDAS Group. Geomagnetic field variations from some equatorial electrojet stations. Sun and Geosphere, 2011;1819-0839:6(2):39–43.

Abbas M, Joshua B, Bonde D, Adimula IA, Rabiu AB, Bello OR. Variability of Electrojet Strength along the Magnetic Equator using MAGDAS/CPMN Data, Journal of Information and Data Management. 2012;1(1):10-13.

Geoscience Australia: Tabulated IQD and IDD data; 2009.

Available:www.ga.gov.au;

Rabiu AB, Mamukuyomi AI, Joshua EO. Variability of equatorial ionosphere inferred from geomagnetic field measurements. Bull. Astr. Soc. India. 2007;35:607-618.

Fambitakoye O,Mayaud PN. Equatorial electrojet and regular daily variation sr- i. a determination of the equatorial electrojet parameters. Journal of Atmospheric and Terrestrial Physics. 1976;38:1-17.

Obiekezie TN,Obiadazie SC. The variation of H component of geomagnetic field at the Africa sector. Physical review & research international. 2013;3(2):154-160.

Onwumechilli CA. The Equatorial Electrojet. Gordon & Breach, Netherlands.1997;627.