13 citations as recorded by crossref.

1. Equatorial plasma fountain and its effects over three locations: Evidence for an additional layer, the F3 layer https://doi.org/10.1029/95JA02639
2. A plasma temperature anomaly in the equatorial topside ionosphere N. Balan et al. https://doi.org/10.1029/97JA00039
3. Simultaneous radar observations of meter‐scale F region irregularities at and off the magnetic equator over India A. Patra et al. https://doi.org/10.1029/2004JA010565
4. Seasonal and solar cycle variability in F‐region vertical plasma drifts over Ouagadougou O. Oyekola et al. https://doi.org/10.1029/2007JA012560
5. Solar eclipse‐induced E‐region plasma irregularities observed by the Gadanki radar A. Patra et al. https://doi.org/10.1029/2009GL038669
6. A comparison of ground and satellite observations of F region vertical velocity near the dip equator O. Oyekola et al. https://doi.org/10.1029/2007RS003699
7. Small‐scale (∼3 m) E region irregularities at and off the magnetic equator B. Murthy et al. https://doi.org/10.1029/98JA00928
8. Comparison between nighttime ionosonde, incoherent scatter radar, AE‐E satellite, and HF Doppler observations ofFregion vertical electrodynamic plasma drifts in the vicinity of the magnetic equator O. Oyekola https://doi.org/10.1029/2006JA011844
9. Solar and geomagnetic trends of equatorial evening and nighttime F region vertical ion drifts O. Oyekola & C. Oluwafemi https://doi.org/10.1029/2008JA013315
10. Radar and satellite global equatorial F region vertical drift model L. Scherliess & B. Fejer https://doi.org/10.1029/1999JA900025
11. Statistical characteristics of VHF radar observations of low latitude E-region field-aligned irregularities over Gadanki A. Patra et al. https://doi.org/10.1016/j.jastp.2004.07.032
12. Equatorial E and F region zonal electric fields in the postsunset period S. Hari et al. https://doi.org/10.1029/95JA03855
13. Radar observations of updrafting and downdrafting plasma depletions associated with the equatorial spread F P. Rao et al. https://doi.org/10.1029/97RS00094