13 citations as recorded by crossref.

1. A complete solar cycle (2006–2016) studies of scale heights derived using COSMIC radio occultation retrieved electron density profiles G. Uma et al. 10.1016/j.jastp.2018.11.010
2. Systematic study of ionospheric scintillation over the indian low-latitudes during low solar activity conditions D. Ayyagari et al. 10.1016/j.asr.2022.07.026
3. Planetary-scale wave structures of the earth’s atmosphere revealed from the COSMIC observations S. Anisetty et al. 10.1007/s13351-014-0101-y
4. Longitudinal structure in electron density at mid-latitudes: upward-propagating tidal effects H. Wang & K. Zhang 10.1186/s40623-016-0596-9
5. Global Longitudinal Behavior of IRI Bottomside Profile Parameters From FORMOSAT‐3/COSMIC Ionospheric Occultations S. Panda et al. 10.1029/2018JA025246
6. Model of the Equatorial Anomaly in foF2 Based on Interkosmos-19 Data for High Solar Activity A. Karpachev & L. Pustovalova 10.1134/S0016793222020104
7. Characterization of African Equatorial Ionization Anomaly During the Maximum Phase of Solar Cycle 24 O. Oyedokun et al. 10.1029/2019JA027066
8. Global Response of the Ionosphere to Atmospheric Tides Forced from Below: Recent Progress Based on Satellite Measurements D. Pancheva & P. Mukhtarov 10.1007/s11214-011-9837-1
9. The Improved Two‐Dimensional Artificial Neural Network‐Based Ionospheric Model (ANNIM) S. Tulasi Ram et al. 10.1029/2018JA025559
10. The day‐to‐day longitudinal variability of the global ionospheric density distribution at low latitudes during low solar activity E. Pacheco & E. Yizengaw 10.1002/jgra.50241
11. Longitudinal and Interhemispheric Ionospheric Response to 2009 and 2013 SSW Events in the African‐European and Indian‐East Asian Sectors G. Kakoti et al. 10.1029/2020JA028570
12. Vertical structure of longitudinal differences in electron densities at mid-latitudes H. Wang et al. 10.1007/s11434-015-0993-7
13. Simulated longitudinal variations in the E-region plasma density induced by non-migrating tides Z. Ren et al. 10.1016/j.jastp.2011.12.004