Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approach
Descripción del Articulo
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...
Autores: | , , , , , , , , , |
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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 |
format |
article |
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 |
dc.rights.uri.none.fl_str_mv |
https://creativecommons.org/licenses/by/4.0/ |
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 |
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Instituto Geofísico del Perú |
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IGP |
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IGP |
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IGP-Institucional |
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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. Subsequently, the geomagnetic storm produced a super fountain effect at the EquatorialIonization Anomaly resulting in the enhancement of foF2.Por paresapplication/pdfengAdvancing Earth and Space Scienceurn:issn:2333-5084info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/4.0/IonosphericGeomagnetic stormSpace weatherMulti-instrumentationEquatorial ionization anomalyhttps://purl.org/pe-repo/ocde/ford#1.03.08Global and regional ionospheric response to a moderate storm in South America and Antarctica using a multi‐instrumental approachinfo:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.igp.gob.pe/bitstreams/30a61946-ad87-4b48-9ff1-89164c8e1902/downloadbb9bdc0b3349e4284e09149f943790b4MD51ORIGINALMelendi_et_al_2025_ESC.pdfMelendi_et_al_2025_ESC.pdfapplication/pdf2428741https://repositorio.igp.gob.pe/bitstreams/dc867cbc-7265-4421-a073-7733eb5324fe/downloadfc1597a3e2896ff212d3e8cc3d0f975fMD52TEXTMelendi_et_al_2025_ESC.pdf.txtMelendi_et_al_2025_ESC.pdf.txtExtracted texttext/plain70801https://repositorio.igp.gob.pe/bitstreams/11b8f83c-d899-4ead-adf4-b1f1f7f61a06/download9f5ed2ac38d798dea34904198f5906eaMD53THUMBNAILMelendi_et_al_2025_ESC.pdf.jpgMelendi_et_al_2025_ESC.pdf.jpgGenerated Thumbnailimage/jpeg49579https://repositorio.igp.gob.pe/bitstreams/45d91a17-a4f5-4031-8abb-ea70e7cba930/downloadf3649f27ea2a02d4aee0dbe0eb05ff97MD5420.500.12816/5738oai:repositorio.igp.gob.pe:20.500.12816/57382025-08-27 17:00:36.018https://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccessopen.accesshttps://repositorio.igp.gob.peRepositorio Geofísico Nacionalbiblio@igp.gob.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 |
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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).