@Article{SantosBBSASCDJVN:2022:CaSt,
author = "Santos, Angela Machado dos and Brum, C. G. M. and Batista, Inez
Staciarini and Sobral, Jos{\'e} Humberto Andrade and Abdu,
Mangalathayil Ali and Souza, Jonas Rodrigues de and Chen, Sony Su
and Denardini, Clezio Marcos and Jesus, Rodolfo de and Venkatesh,
K. and Nogueira, Paulo A. B.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Arecibo
Observatory} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Physical Research Laboratory} and Instituto Federal
de Educa{\c{c}}{\~a}o, Ci{\^e}ncia e Tecnologia de S{\~a}o
Paulo (IFSP)",
title = "Anomalous Responses of the F-2 Layer Over the Brazilian Equatorial
Sector During a Counter Electrojet Event: A Case Study",
journal = "Journal of Geophysical Research: Space Physics",
year = "2022",
volume = "127",
number = "9",
pages = "e2022JA030584",
month = "Sept.",
keywords = "gravity wave, counter electrojet.",
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 Sao Luis (2.33 degrees S; 44
degrees W; I: -4751 degrees; Dip. Lat. 238 degrees 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 Sao
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 Sao Luis and Fortaleza and the
remarkable signatures in ionograms over both regions, such as the
forking traces that are typically caused by GWs.",
doi = "10.1029/2022JA030584",
url = "http://dx.doi.org/10.1029/2022JA030584",
issn = "2169-9402",
language = "en",
targetfile = "JGR Space Physics - 2022 - Santos - Anomalous Responses of the F2
Layer Over the Brazilian Equatorial Sector During a.pdf",
urlaccessdate = "01 maio 2024"
}