@InProceedings{CândidoBKSCOBA:2022:OvBrLo,
author = "C{\^a}ndido, Cl{\'a}udia and Becker Guedes, F{\'a}bio and
Klausner, Virginia and Santos, Stella Moraes and Chingarandi,
Frank Simbarashe and Olusayo, Osanyin Taiwo and Orue and Yenca and
Migoya and Borries, Claudia and Abaidoo, Samuel",
affiliation = "{Universidade do Vale do Para{\'{\i}}ba (UNIVAP)} 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
{Abdus Salam International Center for Theoretical Physics} and
{German Aerospace Center (DLR)} and {Universidade do Vale do
Para{\'{\i}}ba (UNIVAP)}",
title = "An overview of the brazilian low latitude ionospheric response to
space weather events during the declining phase of solar cycle
24",
year = "2022",
organization = "COSPAR Scientific Assembly, 44.",
abstract = "This study shows an overview of the Brazilian low-latitude
ionospheric response during the declining phase and solar minimum
of solar cycle 24. It is well-known that during the descending
phase, solar low-latitude coronal holes are responsible by solar
wind high-speed streams, HSSs, and corotating interaction regions
CIRs-driven geomagnetic storms. Although distinct in nature,
intensity, and duration of their counterpart Coronal Mass
Ejection, CMEs/ICMEsstorms, these solar events can significantly
change the low-latitude ionosphere for several days. By using
multiple ground-based and satellite instrumental techniques, we
analyzed the variation of the Total Electron Content, TEC, its
deviation from the quietest average days behavior, and other
ionospheric parameters and indices. VTEC intensifications can be
as high as 400.",
conference-location = "Athens, Greece",
conference-year = "16-24 July 2022",
language = "en",
targetfile = "C1.5-0003-22-oral.pdf",
urlaccessdate = "03 maio 2024"
}