Articles | Volume 37, issue 3
https://doi.org/10.5194/angeo-37-273-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/angeo-37-273-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Regular paper
| 
06 May 2019
Regular paper |
| 06 May 2019
| 06 May 2019
Quarterdiurnal signature in sporadic E occurrence rates and comparison with neutral wind shear
Institute for Meteorology, Universität Leipzig, Stephanstr. 3,
04103 Leipzig, Germany
Christina Arras
Helmholtz Centre Potsdam German Research Centre for Geosciences – GFZ, Section 1.1: Space Geodetic Techniques,
Telegrafenberg, 14473 Potsdam, Germany
Christoph Geißler
Institute for Meteorology, Universität Leipzig, Stephanstr. 3,
04103 Leipzig, Germany
Friederike Lilienthal
Institute for Meteorology, Universität Leipzig, Stephanstr. 3,
04103 Leipzig, Germany
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Cited
21 citations as recorded by crossref.
- 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
- Simulation of horizontal sporadic E layer movement driven by atmospheric tides S. Andoh et al. 10.1186/s40623-023-01837-0
- 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
- Numerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity Waves L. Qiu et al. 10.1029/2023EA003030
- Understanding the Diurnal Cycle of Midlatitude Sporadic E. The Role of Metal Atoms C. Haldoupis et al. 10.1029/2023JA031336
- 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
- Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates C. Jacobi et al. 10.5194/ars-20-85-2023
- Altitudinal and Latitudinal Variations in Ionospheric Sporadic‐E Layer Obtained From FORMOSAT‐3/COSMIC Radio Occultation L. Qiu et al. 10.1029/2021JA029454
- Intriguing Aspects of Polar-to-Tropical Mesospheric Teleconnections during the 2018 SSW: A Meteor Radar Network Study S. Eswaraiah et al. 10.3390/atmos14081302
- 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
- Forcing mechanisms of the migrating quarterdiurnal tide C. Geißler et al. 10.5194/angeo-38-527-2020
- 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
- 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
- Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
- 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
- Long-Term Observations of the Thermospheric 6 h Oscillation Revealed by an Incoherent Scatter Radar over Arecibo Y. Gong et al. 10.3390/rs15215098
- On the Necessity of Using <i>foμEs</i> Instead of Foes in Estimating The Intensity and Variability of Sporadic E Layers C. Haldoupis et al. 10.2139/ssrn.3586276
- Gravity-wave-perturbed wind shears derived from SABER temperature observations X. Liu et al. 10.5194/acp-20-14437-2020
- 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
- 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
- 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
20 citations as recorded by crossref.
- 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
- Simulation of horizontal sporadic E layer movement driven by atmospheric tides S. Andoh et al. 10.1186/s40623-023-01837-0
- 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
- Numerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity Waves L. Qiu et al. 10.1029/2023EA003030
- Understanding the Diurnal Cycle of Midlatitude Sporadic E. The Role of Metal Atoms C. Haldoupis et al. 10.1029/2023JA031336
- 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
- Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates C. Jacobi et al. 10.5194/ars-20-85-2023
- Altitudinal and Latitudinal Variations in Ionospheric Sporadic‐E Layer Obtained From FORMOSAT‐3/COSMIC Radio Occultation L. Qiu et al. 10.1029/2021JA029454
- Intriguing Aspects of Polar-to-Tropical Mesospheric Teleconnections during the 2018 SSW: A Meteor Radar Network Study S. Eswaraiah et al. 10.3390/atmos14081302
- 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
- Forcing mechanisms of the migrating quarterdiurnal tide C. Geißler et al. 10.5194/angeo-38-527-2020
- 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
- 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
- Global Structure and Seasonal Variations of the Tidal Amplitude in Sporadic‐E Layer Q. Tang et al. 10.1029/2022JA030711
- 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
- Long-Term Observations of the Thermospheric 6 h Oscillation Revealed by an Incoherent Scatter Radar over Arecibo Y. Gong et al. 10.3390/rs15215098
- On the Necessity of Using <i>foμEs</i> Instead of Foes in Estimating The Intensity and Variability of Sporadic E Layers C. Haldoupis et al. 10.2139/ssrn.3586276
- Gravity-wave-perturbed wind shears derived from SABER temperature observations X. Liu et al. 10.5194/acp-20-14437-2020
- 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
- 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
Latest update: 24 Apr 2024
Short summary
Sporadic E (Es) layers in the Earth's ionosphere are produced by ion convergence due to vertical wind shear in the presence of a horizontal component of the Earth's magnetic field. We present analyses of the 6 h tidal signatures in ES occurrence rates derived from GPS radio observations. Times of maxima in ES agree well with those of negative wind shear obtained from radar observation. The global distribution of ES amplitudes agrees with wind shear amplitudes from numerical modeling.
Sporadic E (Es) layers in the Earth's ionosphere are produced by ion convergence due to vertical...
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