25 citations as recorded by crossref.

1. Tidal wind shear observed by meteor radar and comparison with sporadic E occurrence rates based on GPS radio occultation observations C. Jacobi & C. Arras 10.5194/ars-17-213-2019
2. On the role of tidal winds in the descending of the high type of sporadic layer (Es) F. Conceição-Santos et al. 10.1016/j.asr.2019.11.024
3. Tidelike Periodicities of Ionospheric Sporadic E Observed at Low Latitude Hainan Station G. Wang et al. 10.11728/cjss2013.05.501
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5. Intermediate E-F layer dynamics study in the Brazilian low-latitude sector: observational data and simulations M. Muella et al. 10.3389/fspas.2024.1403154
6. Fast Ionogram Observations of Ascending Thin Layers Locally Transported from the E to F Region at Equatorial and Low Latitudes L. Hu et al. 10.3390/rs14225811
7. Some Differences in the Dynamics of the Intermediate Descending Layers Observed During Periods of Maximum and Minimum Solar Flux A. Santos et al. 10.1029/2019JA027682
8. An Empirical Model of the Sporadic E Layer Intensity Based on COSMIC Radio Occultation Observations J. Niu & H. Fang 10.1029/2022SW003280
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10. Blanketing Sporadic‐E Layer Occurrences Over Santa Maria, a Transition Station From Low to Middle Latitude in the South American Magnetic Anomaly (SAMA) J. Moro et al. 10.1029/2022JA030900
11. Comparative anatomy of the day- and night-time radar echoes from the 130–170km region of the low latitude ionosphere A. Patra & P. Pavan Chaitanya 10.1016/j.asr.2013.07.046
12. Sporadic E tidal variabilities and characteristics observed with the Cyprus Digisonde C. Oikonomou et al. 10.1016/j.jastp.2014.07.014
13. Occurrence features of intermediate descending layer and Sporadic E observed over the higher mid-latitude ionospheric station of Moscow C. Oikonomou et al. 10.1186/s40623-023-01796-6
14. On the role of horizontal wind shears in the generation of F0.5 layers over the dip equatorial location of Thiruvananthapuram: A numerical simulation study N. Mridula & T. Pant 10.1016/j.jastp.2017.02.005
15. Terdiurnal Signature of the Critical Frequency of the Sporadic E Layer in Mid-Latitude Regions Based on Ionosonde Observations . Shaoyu Hou et al. 10.1134/S0016793224600218
16. 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
17. Intermediate descending layer and sporadic E tidelike variability observed over three mid-latitude ionospheric stations C. Oikonomou et al. 10.1016/j.asr.2021.08.038
18. Climatology of the short-period (8-h and 6-h) tides observed by meteor radars at Tromsø and Svalbard D. Pancheva et al. 10.1016/j.jastp.2020.105513
19. Descending ion layer property in the Gadanki radar observations of 150 km echoes and its implication to the echoing phenomenon A. Patra 10.1029/2011JA016805
20. Diurnal variations in characteristics of sporadic layer Eₛ over Irkutsk E. Voronova & K. Ratovsky 10.12737/stp-111202507
21. Low‐latitude Es capable of controlling the onset of equatorial spread F L. Joshi et al. 10.1002/jgra.50189
22. Climatology of intermediate descending layers (or 150 km echoes) over the equatorial and low-latitude regions of Brazil during the deep solar minimum of 2009 Â. dos Santos et al. 10.5194/angeo-37-1005-2019
23. Doppler vertical sounding of the ionosphere at the Akademik Vernadsky station A. Zalizovski et al. 10.33275/1727-7485.1.2020.379
24. The Characteristics of Summer Descending Sporadic E Layer Observed With the Ionosondes in the China Region L. Qiu et al. 10.1029/2020JA028729
25. On the seasonal dependence of intermediate descending layer in low latitudes M. Shaikh & M. Khaleel Abusirdaneh 10.1016/j.jastp.2024.106288