36 citations as recorded by crossref.

1. Understanding the Diurnal Cycle of Midlatitude Sporadic E. The Role of Metal Atoms C. Haldoupis et al. 10.1029/2023JA031336
2. A Case Study of Polar Cap Sporadic-E Layer Associated with TEC Variations Y. Wang et al. 10.3390/rs13071324
3. Formation of sporadic-E (Es) layers under the influence of AGWs evolving in a horizontal shear flow G. Didebulidze et al. 10.1016/j.jastp.2015.09.012
4. On the necessity of using foμEs instead of foEs in estimating the intensity and variability of sporadic E layers C. Haldoupis et al. 10.1016/j.jastp.2020.105327
5. 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
6. Diurnal variations in characteristics of sporadic layer Eₛ over Irkutsk E. Voronova & K. Ratovsky 10.12737/szf-111202507
7. Deriving Ionospheric Sporadic E Intensity From FORMOSAT‐3/COSMIC and FY‐3C Radio Occultation Measurements T. Hu et al. 10.1029/2022SW003214
8. The Impact of the Disturbed Electric Field in the Sporadic E (Es) Layer Development Over Brazilian Region L. Resende et al. 10.1029/2020JA028598
9. Anomalous Sporadic‐E Enhancements and Field‐Aligned Irregularities at Low‐Latitudes During the Intense Geomagnetic Activities on 17–18 March 2015 G. Chen et al. 10.1029/2023JA031856
10. Observations of ionospheric irregularities and its correspondence with sporadic e occurrence over South Korea and Japan P. Mungufeni et al. 10.1016/j.asr.2021.01.013
11. Diurnal variations in characteristics of sporadic layer Eₛ over Irkutsk E. Voronova & K. Ratovsky 10.12737/stp-111202507
12. On the solar cycle dependence of the amplitude modulation characterizing the mid-latitude sporadic E layer diurnal periodicity M. Pezzopane et al. 10.1016/j.jastp.2015.11.010
13. Abnormal behaviour of sporadic E-layer during the total solar eclipse of 22 July 2009 near the crest of EIA over India P. Tiwari et al. 10.1016/j.asr.2019.07.037
14. Simulations of blanketing sporadic E-layer over the Brazilian sector driven by tidal winds L. Araujo Resende et al. 10.1016/j.jastp.2016.12.012
15. Sporadic E morphology based on COSMIC radio occultation data and its relationship with wind shear theory J. Luo et al. 10.1186/s40623-021-01550-w
16. Morphology of Ionospheric Sporadic E Layer Intensity Based on COSMIC Occultation Data in the Midlatitude and Low‐Latitude Regions J. Niu et al. 10.1029/2019JA026828
17. 20 March 2015 solar eclipse influence on sporadic E layer M. Pezzopane et al. 10.1016/j.asr.2015.08.001
18. The Influence of Disturbance Dynamo Electric Field in the Formation of Strong Sporadic E Layers Over Boa Vista, a Low‐Latitude Station in the American Sector L. Resende et al. 10.1029/2019JA027519
19. Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
20. Long‐Term Variations and Residual Trends in the E, F, and Sporadic E (Es) Layer Over Juliusruh, Europe M. Sivakandan et al. 10.1029/2022JA031097
21. 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
22. Statistical study on sporadic sodium layers (SSLs) based on diurnal sodium lidar observations at Beijing, China (40.5 °N, 116 °E) Y. Xia et al. 10.1016/j.jastp.2020.105512
23. Global distribution of neutral wind shear associated with sporadic E layers derived from GAIA H. Shinagawa et al. 10.1002/2016JA023778
24. IMPACT OF METEOROLOGICAL STORMS ON THE E-REGION OF THE IONOSPHERE IN 2017–2018 O. Borchevkina et al. 10.12737/stp-64202011
25. On the influence of solar activity on the mid-latitude sporadic E layer M. Pezzopane et al. 10.1051/swsc/2015031
26. On the Necessity of Using <i>foμEs</i> Instead of Foes in Estimating&nbsp;The Intensity and Variability of Sporadic E Layers C. Haldoupis et al. 10.2139/ssrn.3586276
27. An Empirical Model of the Ionospheric Sporadic E Layer Based on GNSS Radio Occultation Data B. Yu et al. 10.1029/2022SW003113
28. 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
29. Impact of meteorological storms on the E-region of the ionosphere in 2017–2018 O. Borchevkina et al. 10.12737/szf-64202011
30. Disturbances in Sporadic‐E During the Great Solar Eclipse of August 21, 2017 G. Chen et al. 10.1029/2020JA028986
31. 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
32. 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
33. Statistical Characteristics of the Low‐Latitude E‐Region Irregularities Observed by the HCOPAR in South China C. Yan et al. 10.1029/2021JA029972
34. 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
35. 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
36. Establishing the first ionospheric observatory in Kenya: Early results from the NORISK project C. Cesaroni et al. 10.1016/j.asr.2025.01.051