12 citations as recorded by crossref.

1. A 12year comparison of MIDAS and IRI 2007 ionospheric Total Electron Content A. Chartier et al. 10.1016/j.asr.2012.02.014
2. foF2 Diurnal Variability at African Equatorial Stations: Dip Equator Secular Displacement Effect D. Gnabahou et al. 10.4236/ijg.2013.48108
3. Investigation in the Variations of Ionospheric f0F2 due to Sunspot Numbers over Wakkanai using EDA Technique . Muzammil Mushtaq Hussain et al. 10.6000/1927-5129.2017.13.69
4. Transient variations of vertical total electron content at low latitude during the period 2013–2017 O. Hammou Ali et al. 10.1016/j.asr.2021.02.039
5. Transient variations of vertical total electron content over some African stations from 2002 to 2012 A. Shimeis et al. 10.1016/j.asr.2014.07.038
6. Long‐term trend of foF2 at a West African equatorial station linked to greenhouse gas increase and dip equator secular displacement D. Gnabahou et al. 10.1002/jgra.50381
7. Time variations of the total electron content in the Southeast Asian equatorial ionization anomaly for the period 2006–2011 M. Le Huy et al. 10.1016/j.asr.2013.08.003
8. Review of Long-Term Trends in the Equatorial Ionosphere Due the Geomagnetic Field Secular Variations and Its Relevance to Space Weather A. Elias et al. 10.3390/atmos13010040
9. Comparison between IRI-2012, IRI-2016 models and F2 peak parameters in two stations of the EIA in Vietnam during different solar activity periods H. Pham Thi Thu et al. 10.1016/j.asr.2020.07.017
10. A comparison of TEC predicted by IRI-2012 with that measured at three different stations in low latitude Indian region for the years (2010–2012) S. Karia et al. 10.1016/j.asr.2016.10.022
11. Seasonal, Diurnal, and Solar-Cycle Variations of Electron Density at Two West Africa Equatorial Ionization Anomaly Stations F. Ouattara et al. 10.1155/2012/640463
12. foF2 long‐term trend linked to Earth's magnetic field secular variation at a station under the northern crest of the equatorial ionization anomaly H. Pham Thi Thu et al. 10.1002/2015JA021890