Comparison of equatorial GPS-TEC observations over an African station and an American station during the minimum and ascending phases of solar cycle 24

Comparison of equatorial GPS-TEC observations over an African station and an American station during the minimum and ascending phases of solar cycle 24

A. O. Akala1, G. K. Seemala2, P. H. Doherty3, C. E. Valladares3, C. S. Carrano3, J. Espinoza4, and S. Oluyo5

1Department of Physics, University of Lagos, Akoka, Yaba, Lagos, Nigeria, 2Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan, 3Institute for Scientific Research, Boston College, Chestnut Hill, MA, USA, 4Jicamarca Radio Observatory, Lima, Peru, 5Department of Physical Science, Yaba College of Technology, Yaba, Lagos, Nigeria

Ann. Geophys., 31, 2085–2096, 2013 www.ann-geophys.net/31/2085/2013/ doi:10.5194/angeo-31-2085-2013

Correspondence to:

A. O. Akala,
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Key Points:

• Ionosphere (Equatorial ionosphere)

Abstract:

GPS-TEC data were observed at the same local time at two equatorial stations on both longitudes: Lagos (6.52◦ N, 3.4◦ E, 3.04◦ S magnetic latitude), Nigeria; and Pucallpa (8.38◦ S, 74.57◦ W, 4.25◦ N magnetic latitude), Peru during the minimum (2009, 2010) and ascending (2011) phases of solar cycle 24. These data were grouped into daily, seasonal and solar activity sets. The day-to-day variations in vertical TEC (VTEC) recorded the maximum during 14:00– 16:00 LT and minimum during 04:00–06:00 LT at both longitudes. Seasonally, during solar minimum, maximum VTEC values were observed during March equinox and minimum during solstices. However, during the ascending phase of the solar activity, the maximum values were recorded during the December solstice and minimum during the June solstice. VTEC also increased with solar activity at both longitudes. On longitude by longitude comparison, the African GPSstation generally recorded higher VTEC values than the American GPS station. Furthermore, harmonic analysis technique was used to extract the annual and semi annual components of the amplitudes of the TEC series at both stations. The semi-annual variations dominated the TEC series over the African equatorial station, while the annual variations dominated those over the American equatorial station. The GPS-TEC-derived averages for non-storm days were compared with the corresponding values derived by the IRI-2007 with the NeQuick topside option. The NeQuick option of IRI-2007 showed better performance at the American sector than the African sector, but generally underestimating TEC during the early morning hours at both longitudes. 

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