2019
DOI: 10.1016/j.asr.2019.02.002
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Analysis of global TEC prediction performance of IRI-PLAS model

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Cited by 10 publications
(4 citation statements)
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“…1b-k), and they could be observed permanently for several days with slight changes in their form and intensity. Andersson et al (2014) detected a hot spot of energetic electron precipitation E > 300 keV in the SH at geomagnetic latitudes between 55 and 72 • S (that was much less pronounced in the NH) and at geographic longitudes between 150 • W and 60 • E. However, this result is based on nighttime observations, i.e., predominantly autumn-winter observations, when almost no LTEs were detected. Using Polar Orbiting Environmental Satellites (POES) data for the analysis of the South Atlantic Anomaly, Domingos et al (2017) found a particle flux plume located within L = 2.5-3 in the South Atlantic.…”
Section: Discussionmentioning
confidence: 83%
“…1b-k), and they could be observed permanently for several days with slight changes in their form and intensity. Andersson et al (2014) detected a hot spot of energetic electron precipitation E > 300 keV in the SH at geomagnetic latitudes between 55 and 72 • S (that was much less pronounced in the NH) and at geographic longitudes between 150 • W and 60 • E. However, this result is based on nighttime observations, i.e., predominantly autumn-winter observations, when almost no LTEs were detected. Using Polar Orbiting Environmental Satellites (POES) data for the analysis of the South Atlantic Anomaly, Domingos et al (2017) found a particle flux plume located within L = 2.5-3 in the South Atlantic.…”
Section: Discussionmentioning
confidence: 83%
“…4 . This is due to the equatorial ionization anomaly [ [74] , [75] , [76] ]. Addis Ababa is located close to the magnetic equator.…”
Section: Resultsmentioning
confidence: 99%
“…Addis Ababa is located close to the magnetic equator. Therefore, eastward electric fields move the F-region plasma near the magnetic equator upward by ExB drift and poleward along the magnetic field lines due to diffusion, so that the electron density near the magnetic equator decreases [ 74 , 75 ]. The day-to-day variation of the zonal electric field could change the electron density near the magnetic equator.…”
Section: Resultsmentioning
confidence: 99%
“…Many scholars utilize the measured data to evaluate the IRI model, refer to Refs. [33][34][35][36][37][38][39][40][41][42][43]. The literature includes the comparison between the IRI model and the site-measured data, in which the sites are mainly located in the equatorial ionization anomaly (EIA) edge region, and also the comparison with the International GNSS Service (IGS) vertical total electron content (VTEC) maps.…”
Section: Introductionmentioning
confidence: 99%