Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world
Descripción del Articulo
There was a solar event around 1850 UT on 9th November 2004, associated with an abnormally large solar wind flow pressure and large southward interplanetary magnetic field, causing an abnormally large prompt penetration electric field between 1850 and 2100 UT. Abnormally large vertical F-region drif...
Autores: | , , , , , , , , |
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Formato: | artículo |
Fecha de Publicación: | 2012 |
Institución: | Instituto Geofísico del Perú |
Repositorio: | IGP-Institucional |
Lenguaje: | inglés |
OAI Identifier: | oai:repositorio.igp.gob.pe:20.500.12816/3028 |
Enlace del recurso: | http://hdl.handle.net/20.500.12816/3028 https://doi.org/10.1007/s12040-012-0231-5 |
Nivel de acceso: | acceso abierto |
Materia: | Equatorial ionosphere Space weather Geomagnetic storm http://purl.org/pe-repo/ocde/ford#1.05.01 |
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dc.title.none.fl_str_mv |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
title |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
spellingShingle |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world Rastogi, R. G. Equatorial ionosphere Space weather Geomagnetic storm http://purl.org/pe-repo/ocde/ford#1.05.01 |
title_short |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
title_full |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
title_fullStr |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
title_full_unstemmed |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
title_sort |
Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world |
author |
Rastogi, R. G. |
author_facet |
Rastogi, R. G. Chandra, H. Condori, Louis Abdu, M. A. Reinisch, B. Tsunoda, R. T. Prasad, D. S. V. V. D. Pant, T. K. Maruyama, T. |
author_role |
author |
author2 |
Chandra, H. Condori, Louis Abdu, M. A. Reinisch, B. Tsunoda, R. T. Prasad, D. S. V. V. D. Pant, T. K. Maruyama, T. |
author2_role |
author author author author author author author author |
dc.contributor.author.fl_str_mv |
Rastogi, R. G. Chandra, H. Condori, Louis Abdu, M. A. Reinisch, B. Tsunoda, R. T. Prasad, D. S. V. V. D. Pant, T. K. Maruyama, T. |
dc.subject.none.fl_str_mv |
Equatorial ionosphere Space weather Geomagnetic storm |
topic |
Equatorial ionosphere Space weather Geomagnetic storm http://purl.org/pe-repo/ocde/ford#1.05.01 |
dc.subject.ocde.none.fl_str_mv |
http://purl.org/pe-repo/ocde/ford#1.05.01 |
description |
There was a solar event around 1850 UT on 9th November 2004, associated with an abnormally large solar wind flow pressure and large southward interplanetary magnetic field, causing an abnormally large prompt penetration electric field between 1850 and 2100 UT. Abnormally large vertical F-region drifts by Jicamarca backscatter radar were reported associated with the event. The F-region over Jicamarca, Peru (14–16 LT) and Sao Luis, Brazil (16–18 LT) was lifted upward, broken into two portions and the upper one was blown out of the range of the ionosonde. At Fortaleza, an off-equatorial station in Brazil, the F-region was also lifted up but later the foF2 increased due to the flow of ionization from upper layer blown up over the equatorial region. The F-region at Ascension Island (19–21 LT), an off-equatorial station, was lifted up without any deformations till 1915 LT but descended at 1930 LT due to reversal of electric field polarity. At Indian stations, Trivandrum and Waltair (00–02 LT), the F-region was pushed down and later disappeared as a consequence of enhanced westward ionospheric electric field in the night sector. The ionosonde did not receive any echo for a couple of hours till the next sunrise. The F-region at Kototaban (03–05 LT), Indonesia also disappeared after a rapid descend. At Kwajelien (06–08 LT) there was no equatorial type of sporadic-E at 07 to 09 LT due to the westward electric field. |
publishDate |
2012 |
dc.date.accessioned.none.fl_str_mv |
2018-09-21T12:02:42Z |
dc.date.available.none.fl_str_mv |
2018-09-21T12:02:42Z |
dc.date.issued.fl_str_mv |
2012-10 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
dc.identifier.citation.none.fl_str_mv |
Rastogi, R. G., Chandra, H., Condori, L., Abdu, M. A., Reinisch, B., Tsunoda, R. T., ... Maruyama, T. (2012). Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world.==$Journal of Earth System Science, 121$==(5), 1145-1161. https://doi.org/10.1007/s12040-012-0231-5 |
dc.identifier.govdoc.none.fl_str_mv |
index-oti2018 |
dc.identifier.uri.none.fl_str_mv |
http://hdl.handle.net/20.500.12816/3028 |
dc.identifier.journal.none.fl_str_mv |
Journal of Earth System Science |
dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1007/s12040-012-0231-5 |
identifier_str_mv |
Rastogi, R. G., Chandra, H., Condori, L., Abdu, M. A., Reinisch, B., Tsunoda, R. T., ... Maruyama, T. (2012). Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world.==$Journal of Earth System Science, 121$==(5), 1145-1161. https://doi.org/10.1007/s12040-012-0231-5 index-oti2018 Journal of Earth System Science |
url |
http://hdl.handle.net/20.500.12816/3028 https://doi.org/10.1007/s12040-012-0231-5 |
dc.language.iso.none.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.none.fl_str_mv |
urn:issn:0253-4126 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.uri.none.fl_str_mv |
https://creativecommons.org/licences/by/4.0/ |
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openAccess |
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https://creativecommons.org/licences/by/4.0/ |
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Springer Verlag |
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Springer Verlag |
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Rastogi, R. G.Chandra, H.Condori, LouisAbdu, M. A.Reinisch, B.Tsunoda, R. T.Prasad, D. S. V. V. D.Pant, T. K.Maruyama, T.2018-09-21T12:02:42Z2018-09-21T12:02:42Z2012-10Rastogi, R. G., Chandra, H., Condori, L., Abdu, M. A., Reinisch, B., Tsunoda, R. T., ... Maruyama, T. (2012). Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the world.==$Journal of Earth System Science, 121$==(5), 1145-1161. https://doi.org/10.1007/s12040-012-0231-5index-oti2018http://hdl.handle.net/20.500.12816/3028Journal of Earth System Sciencehttps://doi.org/10.1007/s12040-012-0231-5There was a solar event around 1850 UT on 9th November 2004, associated with an abnormally large solar wind flow pressure and large southward interplanetary magnetic field, causing an abnormally large prompt penetration electric field between 1850 and 2100 UT. Abnormally large vertical F-region drifts by Jicamarca backscatter radar were reported associated with the event. The F-region over Jicamarca, Peru (14–16 LT) and Sao Luis, Brazil (16–18 LT) was lifted upward, broken into two portions and the upper one was blown out of the range of the ionosonde. At Fortaleza, an off-equatorial station in Brazil, the F-region was also lifted up but later the foF2 increased due to the flow of ionization from upper layer blown up over the equatorial region. The F-region at Ascension Island (19–21 LT), an off-equatorial station, was lifted up without any deformations till 1915 LT but descended at 1930 LT due to reversal of electric field polarity. At Indian stations, Trivandrum and Waltair (00–02 LT), the F-region was pushed down and later disappeared as a consequence of enhanced westward ionospheric electric field in the night sector. The ionosonde did not receive any echo for a couple of hours till the next sunrise. The F-region at Kototaban (03–05 LT), Indonesia also disappeared after a rapid descend. At Kwajelien (06–08 LT) there was no equatorial type of sporadic-E at 07 to 09 LT due to the westward electric field.Por paresapplication/pdfengSpringer Verlagurn:issn:0253-4126info:eu-repo/semantics/openAccesshttps://creativecommons.org/licences/by/4.0/Equatorial ionosphereSpace weatherGeomagnetic stormhttp://purl.org/pe-repo/ocde/ford#1.05.01Abnormally large magnetospheric electric field on 9 November 2004 and its effect on equatorial ionosphere around the worldinfo:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALrastogi2012.pdfrastogi2012.pdfapplication/pdf2316605https://repositorio.igp.gob.pe/bitstreams/b34c8ab3-e80a-4ba5-949c-34e12bf011e3/downloadda14b5f6068d4de425756009592fd7ecMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.igp.gob.pe/bitstreams/5d76b129-b880-49cd-b598-01e2a64eb92e/download8a4605be74aa9ea9d79846c1fba20a33MD52THUMBNAILrastogi2012.pdf.jpgrastogi2012.pdf.jpgIM Thumbnailimage/jpeg74218https://repositorio.igp.gob.pe/bitstreams/13114e0b-db6b-45b1-a769-6d9f79bb3e6e/download0a5f94351be6960fa44a4104a08695abMD53TEXTrastogi2012.pdf.txtrastogi2012.pdf.txtExtracted texttext/plain45917https://repositorio.igp.gob.pe/bitstreams/86a75b44-f7cb-4248-8f71-20292a3acfe3/download5b6e45e014291c9eeda0fc0ae3a19fb3MD5420.500.12816/3028oai:repositorio.igp.gob.pe:20.500.12816/30282024-10-12 22:18:36.086https://creativecommons.org/licences/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).