96 citations as recorded by crossref.

1. The Signature of Sporadic E of an Equatorial Ionosphere of the Low Latitude Region A. Olalekan David et al.
2. Meteor radar wind over Chung-Li (24.9°N, 121°E), Taiwan, for the period 10-25 November 2012 which includes Leonid meteor shower: Comparison with empirical model and satellite measurements C. Su et al.
3. Sporadic E tidal variabilities and characteristics observed with the Cyprus Digisonde C. Oikonomou et al.
4. Derivation of global ionospheric Sporadic E critical frequency ( f o Es) data from the amplitude variations in GPS/GNSS radio occultations B. Yu et al.
5. Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates C. Jacobi et al.
6. On the Relationship Between E Region Scintillation and ENSO Observed by FORMOSAT‐3/COSMIC L. Chang et al.
7. Coordinated sporadic E layer observations made with Chung-Li 30MHz radar, ionosonde and FORMOSAT-3/COSMIC satellites Y. Chu et al.
8. Comprehensive study of sporadic-E formation and time evolution using wind shear theory, radio occultation, and distributed ionosonde observations K. Masjedjamei & A. Mahmoudian
9. Wavenumber‐4 Patterns of the Sporadic E Over the Middle‐ and Low‐Latitudes Z. Liu et al.
10. Morphology and dynamics of daytime mid-latitude sporadic-E patches revealed by GPS total electron content observations in Japan J. Maeda & K. Heki
11. Study of sporadic E layers based on GPS radio occultation measurements and digisonde data over the Brazilian region L. Resende et al.
12. The Mid‐ to High‐Latitude Migrating Semidiurnal Tide: Results From a Mechanistic Tide Model and SuperDARN Observations W. van Caspel et al.
13. Effects of the Northern Hemisphere sudden stratospheric warmings on the Sporadic-E layers in the Brazilian sector P. Fontes et al.
14. Statistically analyzing the effect of ionospheric irregularity on GNSS radio occultation atmospheric measurement M. Li & X. Yue
15. Dynamics of Mid‐Latitude Sporadic‐E and Its Impact on HF Propagation in the North American Sector B. Kunduri et al.
16. Strong Sporadic E Occurrence Detected by Ground‐Based GNSS W. Sun et al.
17. On the necessity of using foμEs instead of foEs in estimating the intensity and variability of sporadic E layers C. Haldoupis et al.
18. The Evolution of Complex Es Observed by Multi Instruments Over Low‐Latitude China W. Sun et al.
19. Statistical study of medium-scale traveling ionospheric disturbances in low-latitude ionosphere using an automatic algorithm P. Cheng et al.
20. Numerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity Waves L. Qiu et al.
21. Quiet and Disturbed Time Characteristics of Blanketing Es (Esb) During Solar Cycle 23 V. Yadav et al.
22. Variation Characteristics of the Ionospheric E Layer over the Tibetan Plateau and Surrounding Areas During a Full Solar Cycle H. Tang et al.
23. Global morphology of ionospheric sporadic E layer from the FormoSat-3/COSMIC GPS radio occultation experiment L. Tsai et al.
24. Electron density retrieval from occulting GNSS signals using a gradient-aided inversion technique I. Kulikov et al.
25. Morphology of Ionospheric Sporadic E Layer Intensity Based on COSMIC Occultation Data in the Midlatitude and Low‐Latitude Regions J. Niu et al.
26. Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al.
27. An Empirical Model of the Ionospheric Sporadic E Layer Based on GNSS Radio Occultation Data B. Yu et al.
28. Ionospheric electron density modelling using B-splines and constraint optimization G. Lalgudi Gopalakrishnan & M. Schmidt
29. 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.
30. Satellite observations of middle atmosphere–thermosphere vertical coupling by gravity waves Q. Trinh et al.
31. Autonomous identification and classification of ionospheric sporadicEin digital ionograms P. Ghosh & F. Berkey
32. Characterizing global equatorial sporadic-E layers through COSMIC GNSS radio occultation measurements A. Seif & S. Panda
33. Variation characteristics of sporadic-E layer in East Asia based on long-term data H. Zhao et al.
34. Ionospheric S4 Scintillations from GNSS Radio Occultation (RO) at Slant Path D. Wu
35. 6 year mean prevailing winds and tides measured by VHF meteor radar over Collm (51.3°N, 13.0°E) C. Jacobi
36. Ionospheric irregularity reconstruction using multisource data fusion via deep learning P. Tian et al.
37. Understanding the Diurnal Cycle of Midlatitude Sporadic E. The Role of Metal Atoms C. Haldoupis et al.
38. Diurnal variations in characteristics of sporadic layer Eₛ over Irkutsk E. Voronova & K. Ratovsky
39. Case study on complex sporadic E layers observed by GPS radio occultations X. Yue et al.
40. Daytime twin-peak structures observed at southern African and European middle latitudes on 8–13 April 2012 Z. Katamzi et al.
41. An attempt to inverse the ionospheric sporadic-E layer critical frequency based on the COSMIC radio occultation data J. Niu et al.
42. Numerical Investigation on the Height and Intensity Variations of Sporadic E Layers at Mid‐Latitude L. Qiu et al.
43. On the occurrence of F region irregularities over Haikou retrieved from COSMIC GPS radio occultation and ground‐based ionospheric scintillation monitor observations X. Yu et al.
44. Estimation Model of Global Ionospheric Irregularities: An Artificial Intelligence Approach P. Tian et al.
45. New global electron density observations from GPS-RO in the D- and E-Region ionosphere D. Wu
46. Diurnal variations in characteristics of sporadic layer Eₛ over Irkutsk E. Voronova & K. Ratovsky
47. Two-dimensional observations of midlatitude sporadicEirregularities with a dense GPS array in Japan J. Maeda & K. Heki
48. Long‐Term Variations and Residual Trends in the E, F, and Sporadic E (Es) Layer Over Juliusruh, Europe M. Sivakandan et al.
49. Enhanced sporadic &lt;i&gt;E&lt;/i&gt; occurrence rates during the Geminid meteor showers 2006–2010 C. Jacobi et al.
50. Sounding of sporadic E layers from China Seismo-Electromagnetic Satellite (CSES) radio occultation and comparing with ionosonde measurements C. Gan et al.
51. The 8-h tide in the mesosphere and lower thermosphere over Collm (51.3° N; 13.0° E), 2004–2011 C. Jacobi & T. Fytterer
52. Global distribution of neutral wind shear associated with sporadic E layers derived from GAIA H. Shinagawa et al.
53. Occurrence and Variations of Middle and Low Latitude Sporadic E Layer Investigated With Longitudinal and Latitudinal Chains of Ionosondes Q. Tang et al.
54. Global distribution of the migrating terdiurnal tide seen in sporadic E occurrence frequencies obtained from GPS radio occultations T. Fytterer et al.
55. Coherent structures in the Es layer and neutral middle atmosphere Z. Mošna et al.
56. 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.
57. Concept of Sporadic E Monitoring Using Space-Based Low Power Multiple Beacon-Systems J. Vanhamel et al.
58. Principle of Locality and Analysis of Radio Occultation Data A. Pavelyev et al.
59. The influence of tidal winds in the formation of blanketing sporadic e-layer over equatorial Brazilian region L. Resende et al.
60. Occurrences of Regional Strong Es Irregularities and Corresponding Scintillations Characterized Using a High‐Temporal‐Resolution GNSS Network W. Sun et al.
61. Retrospect and prospect of ionospheric weather observed by FORMOSAT-3/COSMIC and FORMOSAT-7/COSMIC-2 T. Liu et al.
62. GNSS-RO residual ionospheric error (RIE): a new method and assessment D. Wu et al.
63. Gravity-wave-perturbed wind shears derived from SABER temperature observations X. Liu et al.
64. Comparative Study of the Es Layer between the Plateau and Plain Regions in China W. Wang et al.
65. Sporadic E morphology of East Asia H. Zhao et al.
66. Difference in the Sporadic E Layer Occurrence Ratio Between the Southern and Northern Low Magnetic Latitude Regions as Observed by COSMIC Radio Occultation Data J. Niu
67. Quarterdiurnal signature in sporadic E occurrence rates and comparison with neutral wind shear C. Jacobi et al.
68. Exploring Earth's atmosphere with radio occultation: contributions to weather, climate and space weather R. Anthes
69. Terdiurnal signatures in sporadic &lt;i&gt;E&lt;/i&gt; layers at midlatitudes T. Fytterer et al.
70. Coupling between parameters of Es layer and planetary waves during SSW 2008, 2010 N. Korenkova et al.
71. Formation of sporadic-E (Es) layers under the influence of AGWs evolving in a horizontal shear flow G. Didebulidze et al.
72. An Empirical Model of the Sporadic E Layer Intensity Based on COSMIC Radio Occultation Observations J. Niu & H. Fang
73. Occurrence features of intermediate descending layer and Sporadic E observed over the higher mid-latitude ionospheric station of Moscow C. Oikonomou et al.
74. Gravity wave momentum fluxes in the MLT—Part I: Seasonal variation at Collm (51.3°N, 13.0°E) M. Placke et al.
75. Examining the Wind Shear Theory of Sporadic E With ICON/MIGHTI Winds and COSMIC‐2 Radio Occultation Data Y. Yamazaki et al.
76. Evidence of anti-correlation between sporadic (Es) layers occurrence and solar activity observed at low latitudes over the Brazilian sector P. Fontes et al.
77. Effects of the terdiurnal tide on the sporadic E (Es) layer development at low latitudes over the Brazilian sector P. Fontes et al.
78. Investigating wind shear theory associated with Sporadic-E layer formation using WACCM-X and HWM models, ionosondes, and radio occultation K. Jamei & A. Mahmoudian
79. On the role of tidal winds in the descending of the high type of sporadic layer (Esh) F. Conceição-Santos et al.
80. Estimation of ionospheric sporadic E intensities from GPS radio occultation measurements C. Arras & J. Wickert
81. Midlatitude Sporadic E. A Typical Paradigm of Atmosphere-Ionosphere Coupling C. Haldoupis
82. Analysis of the Sporadic-E Layer Behavior in Different American Stations during the Days around the September 2017 Geomagnetic Storm L. Resende et al.
83. Morphology of sporadic E layer retrieved from COSMIC GPS radio occultation measurements: Wind shear theory examination Y. Chu et al.
84. Characteristics of sporadic E layer in Japan based on multi-station detection J. Feng et al.
85. Global Response of the Ionosphere to Atmospheric Tides Forced from Below: Recent Progress Based on Satellite Measurements D. Pancheva & P. Mukhtarov
86. 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
87. The Occurrence of Sporadic-E Layer over Equatorial Anomaly Crest Region Bhopal . Hafsa Siddiqui et al.
88. Simulations of blanketing sporadic E-layer over the Brazilian sector driven by tidal winds L. Araujo Resende et al.
89. Tidal wind shear observed by meteor radar and comparison with sporadic E occurrence rates based on GPS radio occultation observations C. Jacobi & C. Arras
90. Longitudinal Structure in the Altitude of the Sporadic E Observed by COSMIC in Low-Latitudes Z. Liu et al.
91. Sporadic Structures in the Equatorial Ionosphere from the GPS—Formosat-3 Radio-Occultation Experiments S. Matyugov et al.
92. Deriving Ionospheric Sporadic E Intensity From FORMOSAT‐3/COSMIC and FY‐3C Radio Occultation Measurements T. Hu et al.
93. Interferometry Observations of the Gravity Wave Effect on the Sporadic E Layer C. Seid et al.
94. A Case Study of the Solar and Lunar Semidiurnal Tide Response to the 2013 Sudden Stratospheric Warming W. van Caspel et al.
95. EsTRACE—Es-Layer TRAnsient Cloud Explorer: PlanarSat Mission Concept and Early-Phase Design (Bid, CoDR, PDR) for Sporadic-E Sensing M. Uludağ & A. Aslan
96. Occurrence of pre-sunset L-band scintillation due to strong presence of sporadic-E over Arabian Peninsula M. Shaikh et al.