Articles | Volume 8, issue 1
https://doi.org/10.5194/amt-8-225-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amt-8-225-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Case study on complex sporadic E layers observed by GPS radio occultations
X. Yue
CORRESPONDING AUTHOR
COSMIC Program Office, University Corporation for Atmospheric Research, Boulder, CO, USA
W. S. Schreiner
COSMIC Program Office, University Corporation for Atmospheric Research, Boulder, CO, USA
Z. Zeng
COSMIC Program Office, University Corporation for Atmospheric Research, Boulder, CO, USA
Y.-H. Kuo
COSMIC Program Office, University Corporation for Atmospheric Research, Boulder, CO, USA
CAS Key Laboratory of Geospace Environment, Department of Geophysics & Planetary Sciences, University of Science & Technology of China, Hefei, Anhui, China
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43 citations as recorded by crossref.
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- The Possible Role of Turbopause on Sporadic‐E Layer Formation at Middle and Low Latitudes Q. Tang et al. 10.1029/2021SW002883
- A Statistical Analysis of Sporadic-E Characteristics Associated with GNSS Radio Occultation Phase and Amplitude Scintillations D. Emmons et al. 10.3390/atmos13122098
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- Comparison of middle- and low-latitude sodium layer from a ground-based lidar network, the Odin satellite, and WACCM–Na model B. Yu et al. 10.5194/acp-22-11485-2022
- All‐Sky Tracking of Sporadic Field‐Aligned Irregularities as a Novel Probe of Thermospheric Winds J. Helmboldt & G. Taylor 10.1029/2019EA000867
- A statistical analysis of sporadic E layer occurrence in the midlatitude China region C. Zhou et al. 10.1002/2016JA023135
- 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. 10.1098/rsos.200320
- 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
- Characterizing global equatorial sporadic-E layers through COSMIC GNSS radio occultation measurements A. Seif & S. Panda 10.1007/s10509-024-04326-2
- Longitudinal Structure in the Altitude of the Sporadic E Observed by COSMIC in Low-Latitudes Z. Liu et al. 10.3390/rs13224714
- Sounding of sporadic E layers from China Seismo-Electromagnetic Satellite (CSES) radio occultation and comparing with ionosonde measurements C. Gan et al. 10.5194/angeo-40-463-2022
- Sporadic E S Layers at High Latitudes During a Magnetic Storm of March 17, 2015 According to the Vertical and Oblique Ionospheric Sounding Data D. Blagoveshchensky et al. 10.1007/s11141-017-9814-y
- 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
- Interhemispheric transport of metallic ions within ionospheric sporadic <i>E</i> layers by the lower thermospheric meridional circulation B. Yu et al. 10.5194/acp-21-4219-2021
- Occurrence of pre-sunset L-band scintillation due to strong presence of sporadic-E over Arabian Peninsula M. Shaikh et al. 10.1016/j.asr.2020.02.011
- An Empirical Model of the Sporadic E Layer Intensity Based on COSMIC Radio Occultation Observations J. Niu & H. Fang 10.1029/2022SW003280
- Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
- Morphology of sporadic E layers derived from Fengyun-3C GPS radio occultation measurements X. Xu et al. 10.1186/s40623-022-01617-2
- An Empirical Model of the Ionospheric Sporadic E Layer Based on GNSS Radio Occultation Data B. Yu et al. 10.1029/2022SW003113
- Characterizing GPS radio occultation loss of lock due to ionospheric weather X. Yue et al. 10.1002/2015SW001340
- Modulation of sporadic E layers by small-scale atmospheric waves in Earth’s high-latitude ionosphere В. Губенко et al. 10.12737/stp-53201912
- 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 10.1029/2020SW002635
- Deriving Ionospheric Sporadic E Intensity From FORMOSAT‐3/COSMIC and FY‐3C Radio Occultation Measurements T. Hu et al. 10.1029/2022SW003214
- 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
- Modulation of sporadic E layers by small-scale atmospheric waves in Earth’s high-latitude ionosphere В. Губенко et al. 10.12737/szf-53201912
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- Case study of inclined sporadic E layers in the Earth’s ionosphere observed by CHAMP/GPS radio occultations: Coupling between the tilted plasma layers and internal waves V. Gubenko et al. 10.1016/j.asr.2017.10.001
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- Association of Inclined Sporadic E-Layers and Small-Scale Atmospheric Waves in Earth’s Ionosphere V. Gubenko & I. Kirillovich 10.1134/S0010952520030028
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- Comparison of global morphologies of vertical ion convergence and sporadic E occurrence rate L. Qiu et al. 10.1016/j.asr.2019.02.024
- Comparative study of ionospheric sporadic E occurrence rates using SNRnstd and S4 derived from GPS radio occultation L. Tang et al. 10.1007/s10291-023-01464-y
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Short summary
The occurrence of sporadic E (Es) layers has been a hot scientific topic for a long time. GNSS (global navigation satellite system)-based radio occultation (RO) has proven to be a powerful technique for detecting the global Es layers. In this paper, we show some examples of multiple Es layers occurring in one RO event and the occurrence of Es in a broad region during a certain time interval. The results are then evaluated by independent observations such as lidar and ionosondes.
The occurrence of sporadic E (Es) layers has been a hot scientific topic for a long time. GNSS...