Patterns of GPS-TEC variation over low-latitude regions (African sector) during the deep solar minimum (2008 to 2009) and solar maximum (2012 to 2013) phases

被引:49
作者
Tariku, Yekoye Asmare [1 ]
机构
[1] Ambo Univ, Dept Phys, Ambo, Ethiopia
来源
EARTH PLANETS AND SPACE | 2015年 / 67卷
关键词
Vertical TEC; GPS; Low solar activity; High solar activity; Ionosphere; TOTAL ELECTRON-CONTENT; ANOMALY CREST REGION; EQUATORIAL; VALIDATION; MODEL;
D O I
10.1186/s40623-015-0206-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Due to the unique geometry of the geomagnetic fields near the magnetic equator and low-latitude regions, the satellite communication system in the African sector is strongly influenced by the effects resulting from the accumulation of electrons in their ionosphere. Hence, this paper investigates the patterns of the vertical total electron content (VTEC) variation detected by the Global Positioning System (GPS) over low-latitude regions during a very low (2008 to 2009) and a high solar activity (2012 to 2013) phases. The study has been carried out by considering eight ground-based dual-frequency GPS receivers installed recently at different regions in Ethiopia. In this work, the diurnal, monthly, and seasonal variations in the GPS-VTEC have been analyzed. It has been found that the diurnal variability of VTEC has shown minimum values at around 0300 UT (0600 local time (LT)) and maximum values nearly between 1000 and 1300 UT (1300 and 1600 LT) during both the low and the high activity phases. Moreover, the maximum and minimum of monthly mean hourly VTEC values are observed in October and July, respectively, during both the low (2009) and the high solar activity (2012) phases. It has also been depicted that seasonal mean hourly VTEC values have shown maxima and minima in the March equinox and the June solstice, respectively, during both the low and the high solar activity phases.
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页数:9
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共 38 条
  • [1] Comparison of equatorial GPS-TEC observations over an African station and an American station during the minimum and ascending phases of solar cycle 24
    Akala, A. O.
    Seemala, G. K.
    Doherty, P. H.
    Valladares, C. E.
    Carrano, C. S.
    Espinoza, J.
    Oluyo, S.
    [J]. ANNALES GEOPHYSICAE, 2013, 31 (11) : 2085 - 2096
  • [2] [Anonymous], 2011, Global Positioning System-Signals, Measurements, and Performance
  • [3] Validation of IRI-2012 TEC model over Ethiopia during solar minimum (2009) and solar maximum (2013) phases
    Asmare, Yekoye
    Kassa, Tsegaye
    Nigussie, Melessew
    [J]. ADVANCES IN SPACE RESEARCH, 2014, 53 (11) : 1582 - 1594
  • [4] TEC variations during low solar activity period (2005-2007) near the Equatorial Ionospheric Anomaly Crest region in India
    Bagiya, Mala S.
    Joshi, H. P.
    Iyer, K. N.
    Aggarwal, M.
    Ravindran, S.
    Pathan, B. M.
    [J]. ANNALES GEOPHYSICAE, 2009, 27 (03) : 1047 - 1057
  • [5] TEC derived from GPS network in India and comparison with the IRI
    Bhuyan, P. K.
    Borah, Rashmi Rekha
    [J]. ADVANCES IN SPACE RESEARCH, 2007, 39 (05) : 830 - 840
  • [6] LION: A dynamic computer model for the low-latitude ionosphere
    Bittencourt, J. A.
    Pillat, V. G.
    Fagundes, P. R.
    Sahai, Y.
    Pimenta, A. A.
    [J]. ANNALES GEOPHYSICAE, 2007, 25 (11) : 2371 - 2392
  • [7] EFFECT OF IONIZATION TRANSPORT ON EQUATORIAL F-REGION
    BRAMLEY, EN
    PEART, M
    [J]. NATURE, 1965, 206 (4990) : 1245 - &
  • [8] Calibration errors on experimental slant total electron content (TEC) determined with GPS
    Ciraolo, L.
    Azpilicueta, F.
    Brunini, C.
    Meza, A.
    Radicella, S. M.
    [J]. JOURNAL OF GEODESY, 2007, 81 (02) : 111 - 120
  • [9] Total electron content variations in equatorial anomaly region
    D'ujanga, F. M.
    Mubiru, J.
    Twinamasiko, B. F.
    Basalirwa, C.
    Ssenyonga, T. J.
    [J]. ADVANCES IN SPACE RESEARCH, 2012, 50 (04) : 441 - 449
  • [10] Characterization of low latitude GPS-TEC during very low solar activity phase
    Galav, Praveen
    Dashora, N.
    Sharma, S.
    Pandey, R.
    [J]. JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2010, 72 (17) : 1309 - 1317