Quiet-time and storm-time variations of the African equatorial and low latitude ionosphere during 2009-2015

被引:10
作者
Akala, A. O. [1 ,2 ,3 ,4 ]
Adewusi, E. O. [1 ]
机构
[1] Univ Lagos, Dept Phys, Lagos, Nigeria
[2] Univ Lagos, Distance Learning Inst, Lagos, Nigeria
[3] Univ Lagos, Maritime Inst, Lagos, Nigeria
[4] Abdus Salam Int Ctr Theoret Phys, Trieste, Italy
关键词
African low latitude; Ionosphere; Geomagnetic storms; TEC; Irregularities; TOTAL ELECTRON-CONTENT; GEOMAGNETIC STORM; AMPLITUDE SCINTILLATIONS; SPACE WEATHER; SEASONAL-VARIATIONS; ASCENDING PHASES; ECONOMIC-IMPACT; GPS-TEC; IRREGULARITIES; VARIABILITY;
D O I
10.1016/j.asr.2020.05.038
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
This study investigates the quiet-time and storm-time variations of the African equatorial and low latitude ionosphere during 2009-2015. We obtained TEC observation data from four Global Navigation Satellite System (GNSS) stations over the African equatorial and low latitude, namely: Asab (ASAB, geographic coordinates 13.0 degrees N, 42.65 degrees E; geomagnetic coordinates 4.85 degrees N, 114.34 degrees E), Arba Minch University, (ARMI, 6.03 degrees N, 37.56 degrees E; 3.06 degrees S, 109.29 degrees E), Yamoussoukro (YKRO, 6.87 degrees N, 5.24 degrees W; 2.84 degrees S, 67.41 degrees E) and Mbarara (MBAR, 0.60 degrees S, 30.74 degrees E; 10.27 degrees S, 102.36 degrees E). Seven selected major Geomagnetic Storms (GSs) over solar cycle 24 were investigated and the responses of TEC and Rate of change of TEC Index (ROTI) as proxy for ionospheric irregularities to the storms were also studied. We recorded weaker ionospheric plasma density distributions around the magnetic equator (trough) than at the inner flank of the Equatorial Ionization Anomaly (EIA) crests: A clear evidence of EIA formation. Furthermore, hemispherical asymmetry was observed in the latitudinal distribution of TEC, with consistently higher distribution in the Northern Hemisphere (NH) than Southern Hemisphere (SH). TEC and ionospheric irregularities showed clear dependence on solar activity. Negative responses dominated GSs that occurred at night-time and positive effects for those that occurred during the daytime. The enhancement or inhibition of irregularities during GS is strongly dependent on the time of GS unfolding. As previously established, the daily maximum distribution of TEC at 1400-1600 LT and minimum at 0400-0600 LT were validated by this study, using long time (7 years) data. Seasonally, TEC showed semi-annual pattern of variations, with highest values in equinoxes, and lowest in solstices. (C) 2020 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:1441 / 1459
页数:19
相关论文
共 78 条
  • [1] Equatorial spread F/plasma bubble irregularities under storm time disturbance electric fields
    Abdu, M. A.
    [J]. JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2012, 75 : 44 - 56
  • [2] EQUATORIAL IONOSPHERIC ELECTRIC-FIELDS DURING MAGNETOSPHERIC DISTURBANCES - LOCAL TIME LONGITUDE DEPENDENCES FROM RECENT EITS CAMPAIGNS
    ABDU, MA
    BATISTA, IS
    WALKER, GO
    SOBRAL, JHA
    TRIVEDI, NB
    DEPAULA, ER
    [J]. JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1995, 57 (10): : 1065 - 1083
  • [3] Responses of equatorial F region to different geomagnetic storms observed by GPS in the African sector
    Adewale, A. O.
    Oyeyemi, E. O.
    Adeloye, A. B.
    Ngwira, C. M.
    Athieno, R.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2011, 116
  • [4] Characterization of GPS and EGNOS amplitude scintillations over the African equatorial/low-latitude region
    Akala, A. O.
    Oyeyemi, E. O.
    Arowolo, O. A.
    Doherty, P. H.
    [J]. ADVANCES IN SPACE RESEARCH, 2019, 63 (09) : 3062 - 3075
  • [5] Characterization of GNSS amplitude scintillations over Addis Ababa during 2009-2013
    Akala, A. O.
    Ejalonibu, A. H.
    Doherty, P. H.
    Radicella, S. M.
    Groves, K. M.
    Carrano, C. S.
    Bridgwood, C. T.
    Stoneback, R. A.
    [J]. ADVANCES IN SPACE RESEARCH, 2017, 59 (08) : 1969 - 1983
  • [6] Statistics of GNSS amplitude scintillation occurrences over Dakar, Senegal, at varying elevation angles during the maximum phase of solar cycle 24
    Akala, A. O.
    Awoyele, A.
    Doherty, P. H.
    [J]. SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS, 2016, 14 (03): : 233 - 246
  • [7] Climatology of GPS amplitude scintillations over equatorial Africa during the minimum and ascending phases of solar cycle 24
    Akala, A. O.
    Amaeshi, L. L. N.
    Somoye, E. O.
    Idolor, R. O.
    Okoro, E.
    Doherty, P. H.
    Groves, K. M.
    Carrano, C. S.
    Bridgwood, C. T.
    Baki, P.
    D'ujanga, F. M.
    Seemala, G. K.
    [J]. ASTROPHYSICS AND SPACE SCIENCE, 2015, 357 (01)
  • [8] Characterization of GNSS scintillations over Lagos, Nigeria during the minimum and ascending phases (2009-2011) of solar cycle 24
    Akala, A. O.
    Amaeshi, L. L. N.
    Doherty, P. H.
    Groves, K. M.
    Carrano, C. S.
    Bridgwood, C. T.
    Seemala, G. K.
    Somoye, E. O.
    [J]. ADVANCES IN SPACE RESEARCH, 2014, 53 (01) : 37 - 47
  • [9] 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
  • [10] The response of African equatorial GPS-TEC to intense geomagnetic storms during the ascending phase of solar cycle 24
    Akala, A. O.
    Rabiu, A. B.
    Somoye, E. O.
    Oyeyemi, E. O.
    Adeloye, A. B.
    [J]. JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS, 2013, 98 : 50 - 62