Title
A global 3-D electron density reconstruction model based on radio occultation data and neural networks
Date Issued
15 September 2021
Access level
open access
Resource Type
journal article
Author(s)
Habarulema J.B.
Okoh D.
Burešová D.
Rabiu B.
Tshisaphungo M.
Kosch M.
Häggström I.
Erickson P.J.
Publisher(s)
Elsevier Ltd
Abstract
The accurate representation of the ionospheric electron density in 3-dimensions is a challenging problem because of the nature of horizontal and vertical structures on both small and large scales. This paper presents the development of a global three-dimensional (3-D) electron density reconstruction based on radio occultation data during 2006–2019 and neural networks. We demonstrate that the developed model based on COSMIC dataset only is capable of reproducing different ionospheric features when compared to independent datasets from ionosondes and incoherent scatter radars (ISR) in low, middle and high latitude regions. Following some existing modelling efforts based on similar or related datasets and technique we divided the problem into fine resolution grid cells of 5∘×15∘ (geographic latitudes/longitudes) followed by development of the neural network subroutine per cell and later combining all the 864 sub-models to compile one global model. This approach has been demonstrated to be appropriate in enabling neural networks to learn, reproduce and generalise local and global behaviour of the ionospheric electron density. Based on ISR data, the 3D model improves maximum electron density of the F2 layer (NmF2) prediction by 10%–20% compared to IRI 2016 model during quiet conditions. For estimation of ionosonde ordinary critical frequency of the F2 layer (foF2) in 2009 at 1200 UT (universal time), the developed 3-D model gives average root mean square error (RMSE) values of 0.83 MHz, 1.06 MHz and 1.16 MHz compared to the IRI 2016 values of 0.92 MHz, 1.09 MHz and 1.01 MHz over the Africa–European, American and Asian sectors respectively making their performances statistically comparable. Compared to ionosonde data, the IRI 2016 model consistently shows a better performance for the hmF2 modelling results in almost all sectors during the investigated periods.
Volume
221
Language
English
OCDE Knowledge area
Meteorología y ciencias atmosféricas
Scopus EID
2-s2.0-85108300827
Source
Journal of Atmospheric and Solar-Terrestrial Physics
ISSN of the container
13646826
Sponsor(s)
COSMIC radio occultation electron density profiles were obtained from the COSMIC Data Analysis and Archive Centre ( https://cdaac-www.cosmic.ucar.edu/cdaac/cgi_bin/fileFormats.cgi?type=ionPrf ). F10.7 and Kp values were obtained from the OMNIWeb ( https://omniweb.gsfc.nasa.gov/form/dx1.html ). The Jicamarca and Millistone Hill incoherent scatter radar data were obtained from the Madrigal Databases at Cornell ( http://landau.geo.cornell.edu/madrigal/index.html/ ). The Jicamarca Radio Observatory is a facility of the Instituto Geofísico del Perú operated with support from National Science Foundation (NSF) Award AGS-1732209 to Cornell University. Data in this manuscript can be found in the Madrigal database ( http://www.openmadrigal.org ). Tromsø ISR data was accessed from http://portal.eiscat.se/madrigal/cgi-bin/gSimpleUIAccessData.py and is also available at https://madrigal.eiscat.se/madrigal/list . EISCAT is an international association supported by research organisations in China (CRIRP), Finland (SA), Japan (NIPR and ISEE), Norway (NFR), Sweden (VR), and the United Kingdom (UKRI). This paper uses ionospheric data from the USAF NEXION Digisonde network, the NEXION Program Manager is Mark Leahy. Data from the Brazilian Ionosonde network is made available through the EMBRACE program from the National Institute for Space Research (INPE). This work is based on the research supported in part by the National Research Foundation of South Africa (Grant Numbers 116005) and opinions, findings and conclusions or recommendations expressed in this paper are of the author(s), and the NRF accepts no liability whatsoever in this regard. Global Ionospheric Map products in IONEX format are available at ftp://cddis.gsfc.nasa.gov/pub/gps/products/ionex/ ; and the JPL’s maps were used. We acknowledge and thank the IRI model developers which was accessed on http://irimodel.org/ . We appreciate Drs Yuichi Otsuka, Sudarsanam Tulasi Ram, and Gopi Seemala for the ideas and support they gave in the course of this work. J. B. H. thanks the ISSI-Beijing International Team of “Long term ionospheric effects and their associated modelling during extreme space weather events over the African sector” (the team leaders J. B. Habarulema and Q. Wu) for the valuable discussion about part of the results that are included in this paper. COSMIC radio occultation electron density profiles were obtained from the COSMIC Data Analysis and Archive Centre (https://cdaac-www.cosmic.ucar.edu/cdaac/cgi_bin/fileFormats.cgi?type=ionPrf). F10.7 and Kp values were obtained from the OMNIWeb ( https://omniweb.gsfc.nasa.gov/form/dx1.html). The Jicamarca and Millistone Hill incoherent scatter radar data were obtained from the Madrigal Databases at Cornell ( http://landau.geo.cornell.edu/madrigal/index.html/). The Jicamarca Radio Observatory is a facility of the Instituto Geofísico del Perú operated with support from National Science Foundation (NSF) Award AGS-1732209 to Cornell University. Data in this manuscript can be found in the Madrigal database (http://www.openmadrigal.org). Tromsø ISR data was accessed from http://portal.eiscat.se/madrigal/cgi-bin/gSimpleUIAccessData.py and is also available at https://madrigal.eiscat.se/madrigal/list. EISCAT is an international association supported by research organisations in China (CRIRP), Finland (SA), Japan (NIPR and ISEE), Norway (NFR), Sweden (VR), and the United Kingdom (UKRI). This paper uses ionospheric data from the USAF NEXION Digisonde network, the NEXION Program Manager is Mark Leahy. Data from the Brazilian Ionosonde network is made available through the EMBRACE program from the National Institute for Space Research (INPE). This work is based on the research supported in part by the National Research Foundation of South Africa (Grant Numbers 116005) and opinions, findings and conclusions or recommendations expressed in this paper are of the author(s), and the NRF accepts no liability whatsoever in this regard. Global Ionospheric Map products in IONEX format are available at ftp://cddis.gsfc.nasa.gov/pub/gps/products/ionex/; and the JPL's maps were used. We acknowledge and thank the IRI model developers which was accessed on http://irimodel.org/. We appreciate Drs Yuichi Otsuka, Sudarsanam Tulasi Ram, and Gopi Seemala for the ideas and support they gave in the course of this work. J. B. H. thanks the ISSI-Beijing International Team of “Long term ionospheric effects and their associated modelling during extreme space weather events over the African sector” (the team leaders J. B. Habarulema and Q. Wu) for the valuable discussion about part of the results that are included in this paper.
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