Ionospheric F-region observations over American sector during an intense space weather event using multi-instruments

• Published in: Journal of atmospheric and solar-terrestrial physics Vol. 156; pp. 1 - 14
• Main Authors: de Abreu, A.J., Martin, I.M., Fagundes, P.R., Venkatesh, K., Batista, I.S., de Jesus, R., Rockenback, M., Coster, A., Gende, M., Alves, M.A., Wild, M.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-04-2017
• Subjects: Geomagnetic storm; Ionosphere; Ionospheric irregularities; Space weather; Space weather; Geomagnetic storm; Ionosphere; Ionospheric irregularities
• ISSN: 1364-6826; 1879-1824
• DOI: 10.1016/j.jastp.2017.02.009

The critical interaction between the magnetosphere and ionosphere during intense geomagnetic storms continues to be important to space weather studies. In this investigation, we present and discuss the ionospheric F-region observations in the equatorial, low- and mid-latitude regions in both hemispheres over American sector during the intense geomagnetic storm on 01–03 June 2013. The geomagnetic storm reached a minimum Dst of −119nT at 0900 UT on 01 June. For this investigation, we present vertical total electron content (VTEC) and phase fluctuations (in TECU/min) from a chain of 10 GPS stations and the ionospheric parameters foF2 and h′F from a chain of 4 digital ionosonde stations, covering from equatorial to mid-latitudes regions over American sector during the entire storm-time period 31 May–03 June 2013. In addition, the plasma density observed from DMSP satellites is presented. The results obtained show that during the sudden impulse/SSC and throughout the main phase of the storm, a large positive phase was observed in mid-latitudes of the northern hemisphere, which could be due to changes in the thermospheric wind circulation. On the other hand, in the mid-latitudes of the southern hemisphere, no deviations are observed in VTEC and foF2 when compared to the quiet period. During the long recovery phase of the storm on 01–02 June, a north-south asymmetry is observed in the F-region. The study confirms the dominant role of the thermospheric winds on north-south asymmetry in the ionospheric F-region. The ionospheric irregularities are found to be confined in the equatorial region, of the bottomside spread-F type, before and during the geomagnetic storm. It shows that the geomagnetic storm did not affect the generation or suppression of ionospheric irregularities at the stations investigated.
•This paper studies an intense geomagnetic storm that occurred in June 2013.•We use GPS, ionossonde, and satellites observations over American sector.•The study found positive and negative ionospheric phases due to thermospheric winds changes.