2019
DOI: 10.5194/angeo-37-153-2019
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Emergence of a localized total electron content enhancement during the severe geomagnetic storm of 8 September 2017

Abstract: Abstract. In this work, the results of the analysis on total electron content (TEC) data before, during and after the geomagnetic storm of 8 September 2017 are reported. One of the responses to geomagnetic storms due to the southern vertical interplanetary magnetic field (Bz) is the enhancement of the electron density in the ionosphere. Vertical TEC (VTEC) from the Center for Orbit determination in Europe (CODE) along with a statistical method were used to identify positive and/or negative ionospheric storms i… Show more

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Cited by 6 publications
(2 citation statements)
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“…Many applications relying on radio frequency transmission can be impacted by strong ionospheric perturbations [41]. The culmination of the analysed storm took place on 8 September 2017 and was caused by an X-ray solar flare [42]. This was the most powerful flare of the 24 solar cycle and the strongest flare in a decade.…”
Section: Practical Examination Of the Quality Of Ionosphere Modelsmentioning
confidence: 99%
“…Many applications relying on radio frequency transmission can be impacted by strong ionospheric perturbations [41]. The culmination of the analysed storm took place on 8 September 2017 and was caused by an X-ray solar flare [42]. This was the most powerful flare of the 24 solar cycle and the strongest flare in a decade.…”
Section: Practical Examination Of the Quality Of Ionosphere Modelsmentioning
confidence: 99%
“…Indeed, for the positive storm responses in the event shown in this study, there are ∼800% enhancement in the confined regions in the midlatitude, however, for a fair comparison, only the magnitude of peak‐to‐peak variations of EIA crests is displayed in the figures. Though a magnetic storm was recorded during September 7–8, 2017 with lower solar activity period, and it did produce about 240% enhancement of TEC (Sotomayor‐Beltran & Andrade‐Arenas, 2019), the storm was classified as a severe G4 storm with Dst reaching about −150 nT. Further, the peak‐to‐peak variations of the EIA crests by the storm was about a factor of 2.…”
Section: Discussionmentioning
confidence: 99%