TY - JOUR
T1 - The Early Results and Validation of FORMOSAT-7/COSMIC-2 Space Weather Products
T2 - Global Ionospheric Specification and Ne-Aided Abel Electron Density Profile
AU - Lin, Chi Yen
AU - Lin, Charles Chien Hung
AU - Liu, Jann Yenq
AU - Rajesh, P. K.
AU - Matsuo, Tomoko
AU - Chou, Min Yang
AU - Tsai, Ho Fang
AU - Yeh, Wen Hao
N1 - Funding Information:
This work was financially supported by the Center for Astronautical Physics and Engineering (CAPE) from the Featured Area Research Center program within the framework of Higher Education Sprout Project by the Ministry of Education (MOE) in Taiwan. The work is partially supported by the Ministry of Science and Technology (MOST), Taiwan, under projects MOST 108‐2111‐M‐008‐045‐MY2 and 108‐2638‐M‐006‐001‐MY2; by National Space Organization (NSPO) under project NSPO‐S‐108004; and by the National Science Foundation under project AGS‐1848544. The authors gratefully acknowledge the NSPO and Taiwan Analysis Center for COSMIC (TACC) for providing FORMOSAT‐7/COSMIC‐2 data ( https://tacc.cwb.gov.tw/v2/en/index.html ), the International Reference Ionosphere (IRI) working group for providing the Fortran source code of IRI‐2016 ( http://irimodel.org/IRI‐2016/ ), and the International GNSS Service (IGS) for providing the ground‐based GPS data ( http://garner.ucsd.edu ). The authors also thank the eight digisonde data providers (Figure 5 ) for making their data available via the Lowell GIRO Data Center ( http://giro.uml.edu/ ) and Lowell Digisonde International, LLC for providing manual scaling of the ionogram data.
Funding Information:
This work was financially supported by the Center for Astronautical Physics and Engineering (CAPE) from the Featured Area Research Center program within the framework of Higher Education Sprout Project by the Ministry of Education (MOE) in Taiwan. The work is partially supported by the Ministry of Science and Technology (MOST), Taiwan, under projects MOST 108-2111-M-008-045-MY2 and 108-2638-M-006-001-MY2; by National Space Organization (NSPO) under project NSPO-S-108004; and by the National Science Foundation under project AGS-1848544. The authors gratefully acknowledge the NSPO and Taiwan Analysis Center for COSMIC (TACC) for providing FORMOSAT-7/COSMIC-2 data (https://tacc.cwb.gov.tw/v2/en/index.html), the International Reference Ionosphere (IRI) working group for providing the Fortran source code of IRI-2016 (http://irimodel.org/IRI-2016/), and the International GNSS Service (IGS) for providing the ground-based GPS data (http://garner.ucsd.edu). The authors also thank the eight digisonde data providers (Figure 5) for making their data available via the Lowell GIRO Data Center (http://giro.uml.edu/) and Lowell Digisonde International, LLC for providing manual scaling of the ionogram data.
Publisher Copyright:
© 2020. American Geophysical Union. All Rights Reserved.
PY - 2020/10/1
Y1 - 2020/10/1
N2 - The FORMOSAT-7/COSMIC-2 (F7/C2) satellite mission was launched on 25 June 2019 with six low-Earth-orbit satellites and can provide thousands of daily radio occultation (RO) soundings in the low-latitude and midlatitude regions. This study shows the preliminary results of space weather data products based on F7/C2 RO sounding: global ionospheric specification (GIS) electron density and Ne-aided Abel and Abel electron density profiles. GIS is the ionospheric data assimilation product based on the Gauss-Markov Kalman filter, assimilating the ground-based Global Positioning System and space-based F7/C2 RO slant total electron content, providing continuous global three-dimensional electron density distribution. The Ne-aided Abel inversion implements four-dimensional climatological electron density constructed from previous RO observations, which has the advantage of providing altitudinal information on the horizontal gradient to reduce the retrieval error due to the spherical symmetry assumption of the Abel inversion. The comparisons show that climatological structures are consistent with each other above 300 km altitude. Both the Abel electron density profiles and GIS detect electron density variations during a minor geomagnetic storm that occurred within the study period. Moreover, GIS is further capable of reconstructing the variation of equatorial ionization anomaly crests. Detailed validations of all the three products are carried out using manually scaled digisonde NmF2 (hmF2), yielding correlation coefficients of 0.885 (0.885) for both Abel inversions and 0.903 (0.862) for GIS. The results show that both GIS and Ne-aided Abel are reliable products in studying ionosphere climatology, with the additional advantage of GIS for space weather research and day-to-day variations.
AB - The FORMOSAT-7/COSMIC-2 (F7/C2) satellite mission was launched on 25 June 2019 with six low-Earth-orbit satellites and can provide thousands of daily radio occultation (RO) soundings in the low-latitude and midlatitude regions. This study shows the preliminary results of space weather data products based on F7/C2 RO sounding: global ionospheric specification (GIS) electron density and Ne-aided Abel and Abel electron density profiles. GIS is the ionospheric data assimilation product based on the Gauss-Markov Kalman filter, assimilating the ground-based Global Positioning System and space-based F7/C2 RO slant total electron content, providing continuous global three-dimensional electron density distribution. The Ne-aided Abel inversion implements four-dimensional climatological electron density constructed from previous RO observations, which has the advantage of providing altitudinal information on the horizontal gradient to reduce the retrieval error due to the spherical symmetry assumption of the Abel inversion. The comparisons show that climatological structures are consistent with each other above 300 km altitude. Both the Abel electron density profiles and GIS detect electron density variations during a minor geomagnetic storm that occurred within the study period. Moreover, GIS is further capable of reconstructing the variation of equatorial ionization anomaly crests. Detailed validations of all the three products are carried out using manually scaled digisonde NmF2 (hmF2), yielding correlation coefficients of 0.885 (0.885) for both Abel inversions and 0.903 (0.862) for GIS. The results show that both GIS and Ne-aided Abel are reliable products in studying ionosphere climatology, with the additional advantage of GIS for space weather research and day-to-day variations.
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U2 - 10.1029/2020JA028028
DO - 10.1029/2020JA028028
M3 - Article
AN - SCOPUS:85094680850
SN - 2169-9402
VL - 125
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 10
M1 - e2020JA028028
ER -