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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ANGEO</journal-id>
<journal-title-group>
<journal-title>Annales Geophysicae</journal-title>
<abbrev-journal-title abbrev-type="publisher">ANGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Ann. Geophys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1432-0576</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/angeo-31-2085-2013</article-id>
<title-group>
<article-title>Comparison of equatorial GPS-TEC observations over an African station and an American station during the minimum and ascending phases of solar cycle 24</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Akala</surname>
<given-names>A. O.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Seemala</surname>
<given-names>G. K.</given-names>
<ext-link>https://orcid.org/0000-0002-3690-7873</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Doherty</surname>
<given-names>P. H.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Valladares</surname>
<given-names>C. E.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Carrano</surname>
<given-names>C. S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Espinoza</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Oluyo</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, University of Lagos, Akoka, Yaba, Lagos, Nigeria</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute for Scientific Research, Boston College, Chestnut Hill, MA, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Jicamarca Radio Observatory, Lima, Peru</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Physical Science, Yaba College of Technology, Yaba, Lagos, Nigeria</addr-line>
</aff>
<pub-date pub-type="epub">
<day>22</day>
<month>11</month>
<year>2013</year>
</pub-date>
<volume>31</volume>
<issue>11</issue>
<fpage>2085</fpage>
<lpage>2096</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 A. O. Akala et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://angeo.copernicus.org/articles/31/2085/2013/angeo-31-2085-2013.html">This article is available from https://angeo.copernicus.org/articles/31/2085/2013/angeo-31-2085-2013.html</self-uri>
<self-uri xlink:href="https://angeo.copernicus.org/articles/31/2085/2013/angeo-31-2085-2013.pdf">The full text article is available as a PDF file from https://angeo.copernicus.org/articles/31/2085/2013/angeo-31-2085-2013.pdf</self-uri>
<abstract>
<p>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 GPS station 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.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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