12 citations as recorded by crossref.

1. 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
2. Occurrence features of Intermediate Descending Layers [IL] over the equatorial location of Thiruvananthapuram M. N & T. Pant 10.1016/j.asr.2021.12.003
3. Analysis of the Sporadic-E Layer Behavior in Different American Stations during the Days around the September 2017 Geomagnetic Storm L. Resende et al. 10.3390/atmos13101714
4. Responses of intermediate layers to geomagnetic activity during the 2009 deep solar minimum over the Brazilian low-latitude sector Â. Santos et al. 10.5194/angeo-40-259-2022
5. Ionospheric Variability over the Brazilian Equatorial Region during the Minima Solar Cycles 1996 and 2009: Comparison between Observational Data and the IRI Model Â. Santos et al. 10.3390/atmos14010087
6. 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
7. 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
8. 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
9. 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
10. 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
11. The Characteristics of Summer Descending Sporadic E Layer Observed With the Ionosondes in the China Region L. Qiu et al. 10.1029/2020JA028729
12. Low Altitude Tailing Es (LATTE): Analysis of Sporadic‐E Layer Height at Different Latitudes of Middle and Low Region Q. Tang et al. 10.1029/2022SW003323