Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions
- Autores
- de Abreu, Alessandro José; Correia, Emilia; Denardini, Clezio Marcos; de Jesus, Rodolfo; Venkatesh, Kavutarapu; Roberto, M.; Abalde, José Ricardo; Fagundes, Paulo Roberto; Bolzan, Mauŕicio José Alves; Gende, Mauricio Alfredo
- Año de publicación
- 2022
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- We present and discuss the ionospheric F-region observations from equator to the equatorial ionization anomaly (EIA) regions over the South American sector during an intense space weather event occurred between 27 and May 29, 2017. During this geomagnetic storm, the symmetric-H (SYM-H) reached a minimum of −142 nT at ∼0700 UT on May 28, 2017. For this investigation, we analyze the vertical total electron content (VTEC) observations from a chain of nearly 120 Global Positioning System (GPS) stations. Magnetometer measurements obtained at two stations in the low latitude regions are also presented. The observations do not indicate prompt penetration electric field (PPEF) effects in the VTEC variations. Magnetometer's observations over Cuiabá (CBA) and Cachoeira Paulista (CXP) in central west and south parts of Brazil, respectively, have shown a strong cross-correlation with SYM-H in the period between 3 and 48 h. The results also show positive ionospheric storm phase during the recovery phase on May 28, 2017. Positive effect during the recovery phase of the geomagnetic storm is possibly associated with effects of disturbances winds. During the recovery phase, a strong intensification of the EIA took place, possibly related to an additional ionization effect. The VTEC values show differences between the west and east sectors. This indicates that the EIA crest is stronger in the east sector than in the west sector, possibly due to the combination of disturbance wind effects and geomagnetic field geometry where in the east sector the field lines are more inclined.
Fil: de Abreu, Alessandro José. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Instituto Tecnológico de Aeronáutica; Brasil
Fil: Correia, Emilia. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Universidade Presbiteriana Mackenzie; Brasil
Fil: Denardini, Clezio Marcos. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: de Jesus, Rodolfo. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil
Fil: Venkatesh, Kavutarapu. Physical Research Laboratory; India
Fil: Roberto, M.. Instituto Tecnológico de Aeronáutica; Brasil
Fil: Abalde, José Ricardo. Instituto Tecnológico de Aeronáutica; Brasil
Fil: Fagundes, Paulo Roberto. Universidade do Vale do Paraíba; Brasil
Fil: Bolzan, Mauŕicio José Alves. Universidade Federal de Jataí; Brasil
Fil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina - Materia
-
EIA
GEOMAGNETIC STORM
GPS
IONOSPHERE - Nivel de accesibilidad
- acceso embargado
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/149910
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Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditionsde Abreu, Alessandro JoséCorreia, EmiliaDenardini, Clezio Marcosde Jesus, RodolfoVenkatesh, KavutarapuRoberto, M.Abalde, José RicardoFagundes, Paulo RobertoBolzan, Mauŕicio José AlvesGende, Mauricio AlfredoEIAGEOMAGNETIC STORMGPSIONOSPHEREhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We present and discuss the ionospheric F-region observations from equator to the equatorial ionization anomaly (EIA) regions over the South American sector during an intense space weather event occurred between 27 and May 29, 2017. During this geomagnetic storm, the symmetric-H (SYM-H) reached a minimum of −142 nT at ∼0700 UT on May 28, 2017. For this investigation, we analyze the vertical total electron content (VTEC) observations from a chain of nearly 120 Global Positioning System (GPS) stations. Magnetometer measurements obtained at two stations in the low latitude regions are also presented. The observations do not indicate prompt penetration electric field (PPEF) effects in the VTEC variations. Magnetometer's observations over Cuiabá (CBA) and Cachoeira Paulista (CXP) in central west and south parts of Brazil, respectively, have shown a strong cross-correlation with SYM-H in the period between 3 and 48 h. The results also show positive ionospheric storm phase during the recovery phase on May 28, 2017. Positive effect during the recovery phase of the geomagnetic storm is possibly associated with effects of disturbances winds. During the recovery phase, a strong intensification of the EIA took place, possibly related to an additional ionization effect. The VTEC values show differences between the west and east sectors. This indicates that the EIA crest is stronger in the east sector than in the west sector, possibly due to the combination of disturbance wind effects and geomagnetic field geometry where in the east sector the field lines are more inclined.Fil: de Abreu, Alessandro José. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Instituto Tecnológico de Aeronáutica; BrasilFil: Correia, Emilia. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Universidade Presbiteriana Mackenzie; BrasilFil: Denardini, Clezio Marcos. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: de Jesus, Rodolfo. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; BrasilFil: Venkatesh, Kavutarapu. Physical Research Laboratory; IndiaFil: Roberto, M.. Instituto Tecnológico de Aeronáutica; BrasilFil: Abalde, José Ricardo. Instituto Tecnológico de Aeronáutica; BrasilFil: Fagundes, Paulo Roberto. Universidade do Vale do Paraíba; BrasilFil: Bolzan, Mauŕicio José Alves. Universidade Federal de Jataí; BrasilFil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaElsevier2022-01info:eu-repo/date/embargoEnd/2022-07-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/149910de Abreu, Alessandro José; Correia, Emilia; Denardini, Clezio Marcos; de Jesus, Rodolfo; Venkatesh, Kavutarapu; et al.; Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 227; 1-2022; 1-161364-68261879-1824CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1364682621002510info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jastp.2021.105801info:eu-repo/semantics/embargoedAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:44:00Zoai:ri.conicet.gov.ar:11336/149910instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:44:01.166CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
title |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
spellingShingle |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions de Abreu, Alessandro José EIA GEOMAGNETIC STORM GPS IONOSPHERE |
title_short |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
title_full |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
title_fullStr |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
title_full_unstemmed |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
title_sort |
Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions |
dc.creator.none.fl_str_mv |
de Abreu, Alessandro José Correia, Emilia Denardini, Clezio Marcos de Jesus, Rodolfo Venkatesh, Kavutarapu Roberto, M. Abalde, José Ricardo Fagundes, Paulo Roberto Bolzan, Mauŕicio José Alves Gende, Mauricio Alfredo |
author |
de Abreu, Alessandro José |
author_facet |
de Abreu, Alessandro José Correia, Emilia Denardini, Clezio Marcos de Jesus, Rodolfo Venkatesh, Kavutarapu Roberto, M. Abalde, José Ricardo Fagundes, Paulo Roberto Bolzan, Mauŕicio José Alves Gende, Mauricio Alfredo |
author_role |
author |
author2 |
Correia, Emilia Denardini, Clezio Marcos de Jesus, Rodolfo Venkatesh, Kavutarapu Roberto, M. Abalde, José Ricardo Fagundes, Paulo Roberto Bolzan, Mauŕicio José Alves Gende, Mauricio Alfredo |
author2_role |
author author author author author author author author author |
dc.subject.none.fl_str_mv |
EIA GEOMAGNETIC STORM GPS IONOSPHERE |
topic |
EIA GEOMAGNETIC STORM GPS IONOSPHERE |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
We present and discuss the ionospheric F-region observations from equator to the equatorial ionization anomaly (EIA) regions over the South American sector during an intense space weather event occurred between 27 and May 29, 2017. During this geomagnetic storm, the symmetric-H (SYM-H) reached a minimum of −142 nT at ∼0700 UT on May 28, 2017. For this investigation, we analyze the vertical total electron content (VTEC) observations from a chain of nearly 120 Global Positioning System (GPS) stations. Magnetometer measurements obtained at two stations in the low latitude regions are also presented. The observations do not indicate prompt penetration electric field (PPEF) effects in the VTEC variations. Magnetometer's observations over Cuiabá (CBA) and Cachoeira Paulista (CXP) in central west and south parts of Brazil, respectively, have shown a strong cross-correlation with SYM-H in the period between 3 and 48 h. The results also show positive ionospheric storm phase during the recovery phase on May 28, 2017. Positive effect during the recovery phase of the geomagnetic storm is possibly associated with effects of disturbances winds. During the recovery phase, a strong intensification of the EIA took place, possibly related to an additional ionization effect. The VTEC values show differences between the west and east sectors. This indicates that the EIA crest is stronger in the east sector than in the west sector, possibly due to the combination of disturbance wind effects and geomagnetic field geometry where in the east sector the field lines are more inclined. Fil: de Abreu, Alessandro José. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Instituto Tecnológico de Aeronáutica; Brasil Fil: Correia, Emilia. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil. Universidade Presbiteriana Mackenzie; Brasil Fil: Denardini, Clezio Marcos. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil Fil: de Jesus, Rodolfo. Centro de Previsao de Tempo e Estudos Climáticos. Instituto Nacional de Pesquisas Espaciais; Brasil Fil: Venkatesh, Kavutarapu. Physical Research Laboratory; India Fil: Roberto, M.. Instituto Tecnológico de Aeronáutica; Brasil Fil: Abalde, José Ricardo. Instituto Tecnológico de Aeronáutica; Brasil Fil: Fagundes, Paulo Roberto. Universidade do Vale do Paraíba; Brasil Fil: Bolzan, Mauŕicio José Alves. Universidade Federal de Jataí; Brasil Fil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina |
description |
We present and discuss the ionospheric F-region observations from equator to the equatorial ionization anomaly (EIA) regions over the South American sector during an intense space weather event occurred between 27 and May 29, 2017. During this geomagnetic storm, the symmetric-H (SYM-H) reached a minimum of −142 nT at ∼0700 UT on May 28, 2017. For this investigation, we analyze the vertical total electron content (VTEC) observations from a chain of nearly 120 Global Positioning System (GPS) stations. Magnetometer measurements obtained at two stations in the low latitude regions are also presented. The observations do not indicate prompt penetration electric field (PPEF) effects in the VTEC variations. Magnetometer's observations over Cuiabá (CBA) and Cachoeira Paulista (CXP) in central west and south parts of Brazil, respectively, have shown a strong cross-correlation with SYM-H in the period between 3 and 48 h. The results also show positive ionospheric storm phase during the recovery phase on May 28, 2017. Positive effect during the recovery phase of the geomagnetic storm is possibly associated with effects of disturbances winds. During the recovery phase, a strong intensification of the EIA took place, possibly related to an additional ionization effect. The VTEC values show differences between the west and east sectors. This indicates that the EIA crest is stronger in the east sector than in the west sector, possibly due to the combination of disturbance wind effects and geomagnetic field geometry where in the east sector the field lines are more inclined. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022-01 info:eu-repo/date/embargoEnd/2022-07-10 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/149910 de Abreu, Alessandro José; Correia, Emilia; Denardini, Clezio Marcos; de Jesus, Rodolfo; Venkatesh, Kavutarapu; et al.; Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 227; 1-2022; 1-16 1364-6826 1879-1824 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/149910 |
identifier_str_mv |
de Abreu, Alessandro José; Correia, Emilia; Denardini, Clezio Marcos; de Jesus, Rodolfo; Venkatesh, Kavutarapu; et al.; Ionospheric GPS-TEC responses from equatorial region to the EIA crest in the South American sector under intense space weather conditions; Elsevier; Journal of Atmospheric and Solar-Terrestrial Physics; 227; 1-2022; 1-16 1364-6826 1879-1824 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1364682621002510 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jastp.2021.105801 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
eu_rights_str_mv |
embargoedAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Elsevier |
publisher.none.fl_str_mv |
Elsevier |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1844614476347736064 |
score |
13.069144 |