Anomalous Responses of the F2 Layer Over the Brazilian Equatorial Sector During a Counter Electrojet Event: A Case Study. Issue 9 (8th September 2022)

• Record Type: Journal Article
• Authors: Santos, A. M.; Brum, C. G. M.; Batista, I. S.; Sobral, J. H. A.; Abdu, M. A.; Souza, J. R.; Chen, S. S.; Denardini, C. M.; de Jesus, R.; Venkatesh, K.; Nogueira, P. A. B.
• Is Part Of: Journal of geophysical research. Volume 127:Issue 9(2022)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2022-09-08
• Subjects: gravity wave -- counter electrojet; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1029/2022JA030584
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: In this work, we report the ionospheric F ‐layer responses over the Brazilian equatorial sector to a counter electrojet event that occurred during the solar minimum period of June 2009. The data collected by the Digisonde over São Luis (2.33°S; 44°W; I: −4751°; Dip. Lat. 238°S) showed a strong modification in the ionospheric F 2 layer trace, which in this case appeared to be "broken in half." In this process, the first part of the F 2 layer (lower frequency) was thrown down whilst the upper part remained at higher altitudes. Such characteristics occurred simultaneously with an abrupt decrease in the strength of equatorial electrojet and with intensification in the auroral activity. The origin of this phenomenon seems to have a local nature and seems not to be connected to any magnetic disturbance since similar responses were not observed in other longitudinal and latitudinal sectors. Excluding this possibility, we assume that the strong changes observed in the F layer over São Luis had been caused probably by the gravity wave (GW) propagation, as seen in the downward phase propagation of the altitude contours with time over São Luis and Fortaleza and the remarkable signatures in ionograms over both regions, such as the forking traces that are typically caused by GWs. Key Points: Anomalous responses of the ionospheric F layer over Brazil during a counter electrojet (CEJ) event Weakening and subsequent reversal of daytime equatorial electrojetss is noticed during a period of intense gravity wave (GW) activity The ionospheric F 2 layer stratification under a CEJ event probably due to the GW propagation