Inter-Calibration and Statistical Validation of Topside Ionosphere Electron Density Observations Made by CSES-01 Mission

The China Seismo-Electromagnetic Satellite (CSES-01) provides in situ electron density (Ne) observations through Langmuir probes (LPs) in the topside ionosphere since February 2018. CSES-01 is a sun-synchronous satellite probing the ionosphere around two fixed local times (LTs), 14 LT in the daytime sector and 02 LT in the night-time sector, at an altitude of about 500 km. Previous studies evidenced that CSES-01 seems to underestimate Ne measurements with respect to those acquired by similar satellites or obtained from different instruments. To overcome this issue, we calibrated CSES-01 LP Ne observations through Swarm B satellite data, which flies approximately at CSES-01 altitude. As a first step, Swarm B LP Ne observations were calibrated through Faceplate (FP) Ne observations from the same satellite. Such calibration allowed solving the Ne overestimation made by Swarm LP during nighttime for low solar activity. Then, the calibrated Swarm B LP Ne observations were used to calibrate CSES-01 Ne observations on a statistical basis. Finally, the goodness of the proposed calibration procedure was statistically assessed through a comparison with Ne observations by incoherent scatter radars (ISRs) located at Jicamarca, Arecibo, and Millstone Hill. The proposed calibration procedure allowed solving the CSES-01 Ne underestimation issue for both daytime and nighttime sectors and brought CSES-01 Ne observations in agreement with corresponding ones measured by Swarm B, ISRs, and with those modelled by the International Reference Ionosphere (IRI). This is a first fundamental step towards a possible future inclusion of CSES-01 Ne observations in the dataset underlying IRI for the purpose of improving the description of the topside ionosphere made by IRI.

[1]  J. Bouffard,et al.  Swarm Langmuir probes' data quality validation and future improvements , 2022, Geoscientific Instrumentation, Methods and Data Systems.

[2]  I. Pakhotin,et al.  The swarm Langmuir probe ion drift, density and effective mass (SLIDEM) product , 2022, Earth, Planets and Space.

[3]  Vladimir Truhlik,et al.  On the Electron Temperature in the Topside Ionosphere as Seen by Swarm Satellites, Incoherent Scatter Radars, and the International Reference Ionosphere Model , 2021, Remote. Sens..

[4]  D. Bilitza,et al.  A solar activity correction term for the IRI topside electron density model , 2021 .

[5]  P. Gurram,et al.  Climatological study of the ion temperature in the ionosphere as recorded by Millstone Hill incoherent scatter radar and comparison with the IRI model , 2020 .

[6]  B. Nava,et al.  On the link between the topside ionospheric effective scale height and the plasma ambipolar diffusion, theory and preliminary results , 2020, Scientific Reports.

[7]  Wanqiang Yao,et al.  Study on the plasmaspheric Weddell Sea Anomaly based on COSMIC onboard GPS measurements , 2019, Journal of Atmospheric and Solar-Terrestrial Physics.

[8]  M. Pezzopane,et al.  The ESA Swarm mission to help ionospheric modeling: a new NeQuick topside formulation for mid-latitude regions , 2019, Scientific Reports.

[9]  Xiuying Wang,et al.  Preliminary validation of in situ electron density measurements onboard CSES using observations from Swarm Satellites , 2019, Advances in Space Research.

[10]  Chao Liu,et al.  The technology of space plasma in-situ measurement on the China Seismo-Electromagnetic Satellite , 2018, Science China Technological Sciences.

[11]  Xuhui Shen,et al.  The Langmuir Probe onboard CSES: data inversion analysis method and first results , 2018 .

[12]  Yury V. Yasyukevich,et al.  Winter anomaly in NmF2 and TEC: when and where it can occur , 2018 .

[13]  Xuemin Zhang,et al.  The state-of-the-art of the China Seismo-Electromagnetic Satellite mission , 2018 .

[14]  Michael Pezzopane,et al.  Comparison between IRI and preliminary Swarm Langmuir probe measurements during the St. Patrick storm period , 2016, Earth, Planets and Space.

[15]  V. Shubin,et al.  Global median model of the F2-layer peak height based on ionospheric radio-occultation and ground-based Digisonde observations , 2015 .

[16]  Chao Xiong,et al.  Validation of GRACE electron densities by incoherent scatter radar data and estimation of plasma scale height in the topside ionosphere , 2015 .

[17]  Larry H. Brace,et al.  The Use of Langmuir Probes in Non-Maxwellian Space Plasmas , 2013 .

[18]  K. Tapping The 10.7 cm solar radio flux (F10.7) , 2013 .

[19]  L. Parker,et al.  Impact ionization effects on Pioneer Venus Orbiter , 2011 .

[20]  Sandro M. Radicella,et al.  A new version of the NeQuick ionosphere electron density model , 2008 .

[21]  R. Merlino Understanding Langmuir probe current-voltage characteristics , 2007 .

[22]  J. Gunn,et al.  Sensitivity of electron temperature measurements with the tunnel probe to a fast electron component , 2007 .

[23]  P.-L. Blelly,et al.  The ISL Langmuir probe experiment processing onboard DEMETER: Scientific objectives, description and first results , 2006 .

[24]  H. Lühr,et al.  Swarm An Earth Observation Mission investigating Geospace , 2008 .

[25]  H. Mott-Smith STUDIES OF ELECTRIC DISCHARGES IN GASES AT LOW PRESSURES , 1961 .