Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm

Descripción del Articulo

A moderate geomagnetic storm occurred on April 20, 2018. Using vertical total electron content (VTEC) maps provided by the Center for Orbit Determination in Europe, ionospheric responses to the geomagnetic storm could be identified in generated two-dimensional differential VTEC maps. During the day...

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Detalles Bibliográficos
Autor: Sotomayor Beltran, Carlos
Formato: artículo
Fecha de Publicación:2018
Institución:Universidad de Ciencias y Humanidades
Repositorio:UCH-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.uch.edu.pe:uch/305
Enlace del recurso:http://repositorio.uch.edu.pe/handle/uch/305
https://doi.org/10.1155/2018/1986306
https://www.hindawi.com/journals/ijge/2018/1986306/
Nivel de acceso:acceso abierto
Materia:Ionospheric anomalies
Geomagnetic storm
Geomagnetism
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dc.title.en_PE.fl_str_mv Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
title Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
spellingShingle Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
Sotomayor Beltran, Carlos
Ionospheric anomalies
Geomagnetic storm
Geomagnetism
title_short Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
title_full Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
title_fullStr Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
title_full_unstemmed Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
title_sort Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm
author Sotomayor Beltran, Carlos
author_facet Sotomayor Beltran, Carlos
author_role author
dc.contributor.author.fl_str_mv Sotomayor Beltran, Carlos
dc.subject.en.fl_str_mv Ionospheric anomalies
Geomagnetic storm
Geomagnetism
topic Ionospheric anomalies
Geomagnetic storm
Geomagnetism
description A moderate geomagnetic storm occurred on April 20, 2018. Using vertical total electron content (VTEC) maps provided by the Center for Orbit Determination in Europe, ionospheric responses to the geomagnetic storm could be identified in generated two-dimensional differential VTEC maps. During the day of the storm the enhancement of the equatorial ionization anomaly (EIA), product of the super-fountain effect was identified. A localized TEC enhancement (LTE) was also observed to the south of the EIA on April 20, 2018. It was also possible to visualize this LTE in a longitudinal section of the EIA as a third crest. The maximum increment of VTEC for the LTE was 204%. This LTE is quite unique because it happened during the expected solar cycle 24 and 25 minimum, and according to a previous study no LTE observation could be done for the last solar two-cycle minimum. The origin of the observed LTE is suggested to be partly product of the super-fountain effect. Finally, a localized TEC decrement (LTD) was observed towards the end of the day, April 20, 2018. Because this LTD consisted in the disappearance of the northern and southern crests of the EIA and this occurred during the recovery phase of the geomagnetic storm, it can be suggested that the LTD origin is due to the westward disturbance electric field. This mechanism was put forward by a past study that also analyzed the responses to a geomagnetic storm (the 2015 St. Patrick's day storm), being one of the responses the inhibition of both crests of the EIA.
publishDate 2018
dc.date.accessioned.none.fl_str_mv 2019-08-03T15:50:43Z
dc.date.available.none.fl_str_mv 2019-08-03T15:50:43Z
dc.date.issued.fl_str_mv 2018
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.en_PE.fl_str_mv Sotomayor Beltran, C. (2018). Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm, Geomagnetic Storm. International Journal of Geophysics, 2018.
dc.identifier.issn.none.fl_str_mv 1687-885X
1687-8868
dc.identifier.uri.none.fl_str_mv http://repositorio.uch.edu.pe/handle/uch/305
https://doi.org/10.1155/2018/1986306
https://www.hindawi.com/journals/ijge/2018/1986306/
dc.identifier.doi.en_PE.fl_str_mv 10.1155/2018/1986306
dc.identifier.journal.en_PE.fl_str_mv International Journal of Geophysics
dc.identifier.scopus.none.fl_str_mv 2-s2.0-85054371447
identifier_str_mv Sotomayor Beltran, C. (2018). Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm, Geomagnetic Storm. International Journal of Geophysics, 2018.
1687-885X
1687-8868
10.1155/2018/1986306
International Journal of Geophysics
2-s2.0-85054371447
url http://repositorio.uch.edu.pe/handle/uch/305
https://doi.org/10.1155/2018/1986306
https://www.hindawi.com/journals/ijge/2018/1986306/
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/article
dc.relation.ispartof.none.fl_str_mv International Journal of Geophysics
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/
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dc.publisher.en_PE.fl_str_mv Hindawi Limited
dc.source.en_PE.fl_str_mv Repositorio Institucional - UCH
Universidad de Ciencias y Humanidades
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instname_str Universidad de Ciencias y Humanidades
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spelling Sotomayor Beltran, Carlos2019-08-03T15:50:43Z2019-08-03T15:50:43Z2018Sotomayor Beltran, C. (2018). Localized increment and decrement in the total electron content of the ionosphere as a response to the April 20, 2018, geomagnetic storm, Geomagnetic Storm. International Journal of Geophysics, 2018.1687-885X1687-8868http://repositorio.uch.edu.pe/handle/uch/305https://doi.org/10.1155/2018/1986306https://www.hindawi.com/journals/ijge/2018/1986306/10.1155/2018/1986306International Journal of Geophysics2-s2.0-85054371447A moderate geomagnetic storm occurred on April 20, 2018. Using vertical total electron content (VTEC) maps provided by the Center for Orbit Determination in Europe, ionospheric responses to the geomagnetic storm could be identified in generated two-dimensional differential VTEC maps. During the day of the storm the enhancement of the equatorial ionization anomaly (EIA), product of the super-fountain effect was identified. A localized TEC enhancement (LTE) was also observed to the south of the EIA on April 20, 2018. It was also possible to visualize this LTE in a longitudinal section of the EIA as a third crest. The maximum increment of VTEC for the LTE was 204%. This LTE is quite unique because it happened during the expected solar cycle 24 and 25 minimum, and according to a previous study no LTE observation could be done for the last solar two-cycle minimum. The origin of the observed LTE is suggested to be partly product of the super-fountain effect. Finally, a localized TEC decrement (LTD) was observed towards the end of the day, April 20, 2018. Because this LTD consisted in the disappearance of the northern and southern crests of the EIA and this occurred during the recovery phase of the geomagnetic storm, it can be suggested that the LTD origin is due to the westward disturbance electric field. This mechanism was put forward by a past study that also analyzed the responses to a geomagnetic storm (the 2015 St. Patrick's day storm), being one of the responses the inhibition of both crests of the EIA.Submitted by sistemas uch (sistemas@uch.edu.pe) on 2019-08-03T15:50:43Z No. of bitstreams: 1 2018_Sotomayor-Beltran.pdf: 5466444 bytes, checksum: be66eafef26ffd46e54a3f070be68438 (MD5)Made available in DSpace on 2019-08-03T15:50:43Z (GMT). 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