22 citations as recorded by crossref.

1. An Investigation of the Global TEC Behavior from 1999 to 2017 Variations and Deviations M. Kalaee et al. 10.1134/S0016793221080119
2. Investigation of TEC variations over the magnetic equatorial and equatorial anomaly regions of the African sector B. Oryema et al. 10.1016/j.asr.2015.05.037
3. NmF2 and hmF2 measurements at 95° E and 127° E around the EIA northern crest during 2010–2014 B. Kalita et al. 10.1186/s40623-015-0355-3
4. Performance analysis of IRI-2016 model TEC predictions over Northern and Southern Hemispheric IGS stations during descending phase of solar cycle 24 J. de Dieu Nibigira et al. 10.1007/s11600-021-00618-1
5. Performance evaluation of GIM‐TEC assimilation of the IRI‐Plas model at two equatorial stations in the American sector S. Adebiyi et al. 10.1002/2017SW001596
6. A study on ionospheric scintillation near the EIA crest in relation to equatorial electrodynamics S. Chatterjee et al. 10.1002/2013JA019466
7. Conjugate hemisphere ionospheric response to the St. Patrick's Day storms of 2013 and 2015 in the 100°E longitude sector B. Kalita et al. 10.1002/2016JA023119
8. Growth of L-band scintillation at anomaly crest station in association with strong TEC gradient: A study covering wide solar activity period K. Pathak et al. 10.1007/s12648-018-1165-9
9. Ionospheric VTEC variations over Pakistan in the descending phase of solar activity during 2016–17 M. Tariq et al. 10.1007/s10509-019-3591-3
10. Variability of ionospheric TEC at low latitude station, Hyderabad during medium solar activity S. Bhardwaj et al. 10.2205/2020ES000749
11. Nonlinear dependence of ionospheric F2 layer critical frequency on solar activity in southern latitudes during solar cycle 23 C. Seema & P. Prince 10.1016/j.asr.2018.05.031
12. Statistical analysis of the correlation between the equatorial electrojet and the occurrence of the equatorial ionisation anomaly over the East African sector P. Mungufeni et al. 10.5194/angeo-36-841-2018
13. Latitudinal effect on the diurnal variation of the F2 layer at low solar activity J. Adeniyi & B. Joshua 10.1016/j.jastp.2014.09.005
14. An empirical model of ionospheric total electron content (TEC) near the crest of the equatorial ionization anomaly (EIA) R. Hajra et al. 10.1051/swsc/2016023
15. Seasonal and solar cycle effects on TEC at 95°E in the ascending half (2009–2014) of the subdued solar cycle 24: Consistent underestimation by IRI 2012 G. Kakoti et al. 10.1016/j.asr.2016.09.002
16. GPS derived TEC and foF2 variability at an equatorial station and the performance of IRI-model S. Adebiyi et al. 10.1016/j.asr.2014.03.026
17. Ionospheric foF2 variability over the Southeast Asian sector A. Akala et al. 10.1029/2010JA015250
18. Study of daytime vertical E × B drift velocities inferred from ground-based magnetometer observations of ΔH, at low latitudes under geomagnetically disturbed conditions P. Subhadra Devi & K. Unnikrishnan 10.1016/j.asr.2013.12.007
19. F2 layer characteristics and electrojet strength over an equatorial station B. Adebesin et al. 10.1016/j.asr.2013.05.025
20. Coordinated in situ measurements of plasma irregularities and ground based scintillation observations at the crest of equatorial anomaly S. Sarkar & A. Gwal 10.1016/j.asr.2014.01.023
21. The response of the ionosphere over Ilorin to some geomagnetic storms B. Joshua et al. 10.1016/j.asr.2014.08.027
22. An investigation of the ionospheric F region near the EIA crest in India using OI 777.4 and 630.0 nm nightglow observations N. Parihar et al. 10.5194/angeo-36-809-2018