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Diurnal Variation of TEC and S 4 Index During the Period of Low Geomagnetic Activity at Ile-Ife, Nigeria

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Abstract

Ile-Ife lies on the equatorial anomaly region where the ionospheric current is greatly influenced by the existence of the equatorial electrojet. The dual frequency SCINDA NovAtel GSV 4004B GPS receiver recently installed at Ile-Ife [on geographical latitude 7°33′N and longitude 4°33′E and geomagnetic dipole (coordinate) of latitude 9.84°N and longitude 77.25°E] is currently operational and recording data from the available global positioning system satellites. The receiver provides the data on total electron content (TEC) and the scintillation index (S 4). This paper presents the first sets of results from this station. Data records for the month of February 2010 were analyzed using the WinTec-P software program and these were interpreted to discuss the diurnal variation of the TEC and S 4 index during the period considered, as having low geomagnetic activity. The vertical TEC in this study showed that the values vary widely from as low as 0 TECu about sunrise to about 35 TECu during the day. Depletion in TEC was also noticed about sunset and marked by the occurrence of scintillations with a maximum index value of 0.3. Results of the IRI models and the observed TEC differ considerably; hence, there is the need to improve IRI models for its adaptability to the Africa ionospheric conditions.

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Authors and Affiliations

  1. Department of Physics, Obafemi Awolowo University, Ile-Ife, Nigeria

    E. A. Ariyibi

  2. Institute of Scientific Research, Boston College, Boston, USA

    P. Doherty

  3. Haystack Observatory, M.I.T., Westford, USA

    A. J. Coster

  4. Department of Physics, University of Ibadan, Ibadan, Nigeria

    E. O. Joshua

Authors
  1. E. A. Ariyibi
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  2. P. Doherty
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  3. A. J. Coster
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  4. E. O. Joshua
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Correspondence to E. A. Ariyibi.

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Ariyibi, E.A., Doherty, P., Coster, A.J. et al. Diurnal Variation of TEC and S 4 Index During the Period of Low Geomagnetic Activity at Ile-Ife, Nigeria. Arab J Sci Eng 38, 1807–1813 (2013). https://doi.org/10.1007/s13369-012-0420-1

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  • DOI: https://doi.org/10.1007/s13369-012-0420-1

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