23 citations as recorded by crossref.

1. Competition between winds and electric fields in the formation of blanketing sporadic E layers at equatorial regions L. Resende et al. 10.1186/s40623-016-0577-z
2. A Statistical Analysis of Global Ionospheric E‐Layer Scintillation During 2007–2014 Q. Li et al. 10.1029/2018RS006764
3. Occurrence of blanketing E<sub>s</sub> layer (E<sub>sb</sub>) over the equatorial region during the peculiar minimum of solar cycle 24 V. Yadav et al. 10.5194/angeo-32-553-2014
4. Electrodynamical control of the ambient ionization near the equatorial anomaly crest in the Indian zone during counter electrojet days R. Hajra et al. 10.1029/2008RS003904
5. Features of the occurrence of the additional stratification on the bottom-side F region over the equatorial location of Trivandrum N. Mridula et al. 10.1016/j.asr.2013.12.036
6. Equatorial sporadic E-layer abnormal density enhancement during the recovery phase of the December 2006 magnetic storm: A case study L. Resende & C. Denardini 10.5047/eps.2011.10.007
7. On the Linkage Between Daytime E Region Field‐Aligned Irregularities and Sporadic E Layer at Low Latitude B. Sahu et al. 10.1029/2023JA031877
8. Abnormal fb Es enhancements in equatorial Es layers during magnetic storms of solar cycle 23 L. Resende et al. 10.1016/j.jastp.2013.05.020
9. Vertical coupling between the mesopause region and sporadic-E layer during equatorial counter electrojet events – A case study A. Ajesh et al. 10.1016/j.asr.2018.07.001
10. Study of equatorial E region irregularities using rare daytime VHF scintillation observations V. Yadav et al. 10.1002/2015JA021320
11. Quiet and Disturbed Time Characteristics of Blanketing Es (Esb) During Solar Cycle 23 V. Yadav et al. 10.1002/2017JA023911
12. The influence of tidal winds in the formation of blanketing sporadic e-layer over equatorial Brazilian region L. Resende et al. 10.1016/j.jastp.2017.06.009
13. On blanketing sporadic E and polarization effects near the equatorial electrojet R. Tsunoda 10.1029/2008JA013158
14. Different Sporadic‐E (Es) Layer Types Development During the August 2018 Geomagnetic Storm: Evidence of Auroral Type (Esa) Over the SAMA Region J. Moro et al. 10.1029/2021JA029701
15. Ionospheric variability over Indian low latitude linked with the 2009 sudden stratospheric warming A. Patra et al. 10.1002/2014JA019847
16. Occurrence of the blanketing sporadic E layer during the recovery phase of the October 2003 superstorm C. Denardini et al. 10.1186/s40623-016-0456-7
17. Worldwide study of the Sporadic E (Es) layer development during a space weather event L. Resende et al. 10.1016/j.jastp.2022.105966
18. The Impact of the Disturbed Electric Field in the Sporadic E (Es) Layer Development Over Brazilian Region L. Resende et al. 10.1029/2020JA028598
19. F2 layer characteristics and electrojet strength over an equatorial station B. Adebesin et al. 10.1016/j.asr.2013.05.025
20. New Findings of the Sporadic E (Es) Layer Development Around the Magnetic Equator During a High‐Speed Solar (HSS) Wind Stream Event L. Resende et al. 10.1029/2021JA029416
21. Quantifying the EEJ current with ground-based ionosonde inferred vertical E × B drifts in the morning hours over Ilorin, West Africa J. Adeniyi et al. 10.2478/s11600-014-0202-0
22. Day and nighttime L-Band amplitude scintillations during low solar activity at a low latitude station in the South Pacific region R. Prasad & S. Kumar 10.1016/j.jastp.2017.11.005
23. On the solar activity variations of nocturnal F region vertical drifts covering two solar cycles in the Indian longitude sector M. Madhav Haridas et al. 10.1002/2014JA020561