22 citations as recorded by crossref.

1. 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
2. Simulation of horizontal sporadic E layer movement driven by atmospheric tides S. Andoh et al. 10.1186/s40623-023-01837-0
3. Correlation betweenfoEsand zonal winds over Rome, Okinawa and Townsville using Horizontal Wind Model (HWM14) during solar cycle 22 B. Gul et al. 10.1016/j.asr.2021.08.027
4. Numerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity Waves L. Qiu et al. 10.1029/2023EA003030
5. Understanding the Diurnal Cycle of Midlatitude Sporadic E. The Role of Metal Atoms C. Haldoupis et al. 10.1029/2023JA031336
6. Using GNSS radio occultation data to derive critical frequencies of the ionospheric sporadic E layer in real time B. Yu et al. 10.1007/s10291-020-01050-6
7. Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates C. Jacobi et al. 10.5194/ars-20-85-2023
8. Altitudinal and Latitudinal Variations in Ionospheric Sporadic‐E Layer Obtained From FORMOSAT‐3/COSMIC Radio Occultation L. Qiu et al. 10.1029/2021JA029454
9. The Characteristics of Summer Descending Sporadic E Layer Observed With the Ionosondes in the China Region L. Qiu et al. 10.1029/2020JA028729
10. Intriguing Aspects of Polar-to-Tropical Mesospheric Teleconnections during the 2018 SSW: A Meteor Radar Network Study S. Eswaraiah et al. 10.3390/atmos14081302
11. Strong Quarterdiurnal Tides in the Mesosphere and Lower Thermosphere During the 2019 Arctic Sudden Stratospheric Warming Over Mohe, China Y. Gong et al. 10.1029/2020JA029066
12. Forcing mechanisms of the migrating quarterdiurnal tide C. Geißler et al. 10.5194/angeo-38-527-2020
13. 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
14. Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA model S. Sobhkhiz-Miandehi et al. 10.1186/s40623-022-01637-y
15. Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
16. On the altitude dependence and role of zonal and meridional wind shears in the generation of E region metal ion layers C. Haldoupis & S. Shalimov 10.1016/j.jastp.2021.105537
17. Long-Term Observations of the Thermospheric 6 h Oscillation Revealed by an Incoherent Scatter Radar over Arecibo Y. Gong et al. 10.3390/rs15215098
18. 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
19. Gravity-wave-perturbed wind shears derived from SABER temperature observations X. Liu et al. 10.5194/acp-20-14437-2020
20. Relationship Between Wavenumber 4 Pattern of Sporadic E Layer Intensity and Eastward Propagating Diurnal Tide With Zonal Wavenumber 3 in Low Latitude Region J. Niu 10.1029/2020JA028985
21. 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
22. 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