Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach

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In this study, we investigate the ionospheric disturbances caused by a moderate geomagneticstorm (maximum Kp = 6) occurring between 26th February and 1 March 2023. Ionospheric response for thecoupling between the solar wind, magnetosphere, and ionosphere systems can be observed across variousregions...

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Detalles Bibliográficos
Autores: Melendi, Y. D., Bravo, M., Molina, M. G., Paz, M., Urra, B., De Pasquale, L., Scipión, Danny, Namour, J., Duran, T., Zalizovski, A.
Formato: artículo
Fecha de Publicación:2025
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/5738
Enlace del recurso:http://hdl.handle.net/20.500.12816/5738
https://doi.org/10.1029/2025EA004281
Nivel de acceso:acceso abierto
Materia:Ionospheric
Geomagnetic storm
Space weather
Multi-instrumentation
Equatorial ionization anomaly
https://purl.org/pe-repo/ocde/ford#1.03.08
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dc.title.none.fl_str_mv Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
title Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
spellingShingle Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
Melendi, Y. D.
Ionospheric
Geomagnetic storm
Space weather
Multi-instrumentation
Equatorial ionization anomaly
https://purl.org/pe-repo/ocde/ford#1.03.08
title_short Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
title_full Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
title_fullStr Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
title_full_unstemmed Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
title_sort Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
author Melendi, Y. D.
author_facet Melendi, Y. D.
Bravo, M.
Molina, M. G.
Paz, M.
Urra, B.
De Pasquale, L.
Scipión, Danny
Namour, J.
Duran, T.
Zalizovski, A.
author_role author
author2 Bravo, M.
Molina, M. G.
Paz, M.
Urra, B.
De Pasquale, L.
Scipión, Danny
Namour, J.
Duran, T.
Zalizovski, A.
author2_role author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Melendi, Y. D.
Bravo, M.
Molina, M. G.
Paz, M.
Urra, B.
De Pasquale, L.
Scipión, Danny
Namour, J.
Duran, T.
Zalizovski, A.
dc.subject.none.fl_str_mv Ionospheric
Geomagnetic storm
Space weather
Multi-instrumentation
Equatorial ionization anomaly
topic Ionospheric
Geomagnetic storm
Space weather
Multi-instrumentation
Equatorial ionization anomaly
https://purl.org/pe-repo/ocde/ford#1.03.08
dc.subject.ocde.none.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.03.08
description In this study, we investigate the ionospheric disturbances caused by a moderate geomagneticstorm (maximum Kp = 6) occurring between 26th February and 1 March 2023. Ionospheric response for thecoupling between the solar wind, magnetosphere, and ionosphere systems can be observed across variousregions of the globe and it may vary according to the local/regional background ionospheric conditions. Weanalyzed space and ground‐based instruments (e.g., ionosondes, total electron content, GUVI imager,incoherent scatter radar) covering from Antarctica to equatorial latitudes in South America. From a globalperspective, we observed two ionospheric storms. The first, with a negative phase observed as a significantdecrease (>30%) in the F2‐layer critical frequency (foF2), occurred on February 27th at 01:00 UT. This negativephase storm was observed in all the considered regions, with the intensity progressively decreasing from higherto lower latitudes. It is worth mentioning that, for the Antarctic station, we consider the local regime of theWeddell Sea Anomaly. The second ionospheric storm occurred during the recovery phase of the geomagneticstorm on 28th February. In this last case, an enhancement above 30% in foF2 was observed only in the low‐latitude station. Subsequently, the geomagnetic storm produced a super fountain effect at the EquatorialIonization Anomaly resulting in the enhancement of foF2.
publishDate 2025
dc.date.accessioned.none.fl_str_mv 2025-08-27T21:48:06Z
dc.date.available.none.fl_str_mv 2025-08-27T21:48:06Z
dc.date.issued.fl_str_mv 2025-08-20
dc.type.none.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.citation.none.fl_str_mv Melendi, Y. D., Bravo, M., Molina, M. G., Paz, M., Urra, B., De Pasquale, L., … Zalizovski, A. (2025). Global and Regional Ionospheric Response to a Moderate Storm in South America and Antarctica Using a Multi-Instrumental Approach.==$Earth and Space Science, 12$==(8). https://doi.org/10.1029/2025EA004281
dc.identifier.govdoc.none.fl_str_mv index-oti2018
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/20.500.12816/5738
dc.identifier.journal.none.fl_str_mv Earth and Space Sciences
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1029/2025EA004281
identifier_str_mv Melendi, Y. D., Bravo, M., Molina, M. G., Paz, M., Urra, B., De Pasquale, L., … Zalizovski, A. (2025). Global and Regional Ionospheric Response to a Moderate Storm in South America and Antarctica Using a Multi-Instrumental Approach.==$Earth and Space Science, 12$==(8). https://doi.org/10.1029/2025EA004281
index-oti2018
Earth and Space Sciences
url http://hdl.handle.net/20.500.12816/5738
https://doi.org/10.1029/2025EA004281
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:2333-5084
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/4.0/
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Advancing Earth and Space Science
publisher.none.fl_str_mv Advancing Earth and Space Science
dc.source.none.fl_str_mv reponame:IGP-Institucional
instname:Instituto Geofísico del Perú
instacron:IGP
instname_str Instituto Geofísico del Perú
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spelling Melendi, Y. D.Bravo, M.Molina, M. G.Paz, M.Urra, B.De Pasquale, L.Scipión, DannyNamour, J.Duran, T.Zalizovski, A.2025-08-27T21:48:06Z2025-08-27T21:48:06Z2025-08-20Melendi, Y. D., Bravo, M., Molina, M. G., Paz, M., Urra, B., De Pasquale, L., … Zalizovski, A. (2025). Global and Regional Ionospheric Response to a Moderate Storm in South America and Antarctica Using a Multi-Instrumental Approach.==$Earth and Space Science, 12$==(8). https://doi.org/10.1029/2025EA004281index-oti2018http://hdl.handle.net/20.500.12816/5738Earth and Space Scienceshttps://doi.org/10.1029/2025EA004281In this study, we investigate the ionospheric disturbances caused by a moderate geomagneticstorm (maximum Kp = 6) occurring between 26th February and 1 March 2023. Ionospheric response for thecoupling between the solar wind, magnetosphere, and ionosphere systems can be observed across variousregions of the globe and it may vary according to the local/regional background ionospheric conditions. Weanalyzed space and ground‐based instruments (e.g., ionosondes, total electron content, GUVI imager,incoherent scatter radar) covering from Antarctica to equatorial latitudes in South America. From a globalperspective, we observed two ionospheric storms. The first, with a negative phase observed as a significantdecrease (>30%) in the F2‐layer critical frequency (foF2), occurred on February 27th at 01:00 UT. This negativephase storm was observed in all the considered regions, with the intensity progressively decreasing from higherto lower latitudes. It is worth mentioning that, for the Antarctic station, we consider the local regime of theWeddell Sea Anomaly. The second ionospheric storm occurred during the recovery phase of the geomagneticstorm on 28th February. In this last case, an enhancement above 30% in foF2 was observed only in the low‐latitude station. 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