Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004
Descripción del Articulo
By making use of multiple ground‐based and spaceborne instruments, we study ionospheric and thermospheric behavior during the moderately intense geomagnetic storm of 29–31 August 2004 (minimum Dst excursion of −128 nT). Although this storm was far from the strongest in solar cycle 23, it provoked qu...
Autores: | , , |
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Formato: | artículo |
Fecha de Publicación: | 2014 |
Institución: | Instituto Geofísico del Perú |
Repositorio: | IGP-Institucional |
Lenguaje: | inglés |
OAI Identifier: | oai:repositorio.igp.gob.pe:20.500.12816/3692 |
Enlace del recurso: | http://hdl.handle.net/20.500.12816/3692 https://doi.org/10.1002/2014JA020710 |
Nivel de acceso: | acceso abierto |
Materia: | Ionospheric storm Hemispheric asymmetry Topside contribution Superfountain effect Thermospheric storm Postsunset sector http://purl.org/pe-repo/ocde/ford#1.05.01 |
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IGP-Institucional |
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4701 |
dc.title.none.fl_str_mv |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
title |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
spellingShingle |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 Astafyeva, Elvira Ionospheric storm Hemispheric asymmetry Topside contribution Superfountain effect Thermospheric storm Postsunset sector http://purl.org/pe-repo/ocde/ford#1.05.01 |
title_short |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
title_full |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
title_fullStr |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
title_full_unstemmed |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
title_sort |
Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004 |
author |
Astafyeva, Elvira |
author_facet |
Astafyeva, Elvira Zakharenkova, Irina Doornbos, Eelco |
author_role |
author |
author2 |
Zakharenkova, Irina Doornbos, Eelco |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Astafyeva, Elvira Zakharenkova, Irina Doornbos, Eelco |
dc.subject.none.fl_str_mv |
Ionospheric storm Hemispheric asymmetry Topside contribution Superfountain effect Thermospheric storm Postsunset sector |
topic |
Ionospheric storm Hemispheric asymmetry Topside contribution Superfountain effect Thermospheric storm Postsunset sector 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 |
By making use of multiple ground‐based and spaceborne instruments, we study ionospheric and thermospheric behavior during the moderately intense geomagnetic storm of 29–31 August 2004 (minimum Dst excursion of −128 nT). Although this storm was far from the strongest in solar cycle 23, it provoked quite interesting effects in the ionosphere, such as opposite hemispheric asymmetries in the ionospheric F layer and in the topside ionosphere and a development of the ionospheric superfountain effect in the postsunset sector. Data from ground‐based GPS receivers and ionosondes revealed large increase in total electron content (TEC) and in NmF2 in the southern hemisphere, whereas in the northern hemisphere, very weak or no effect was observed. On the contrary, the topside measurements indicated the occurrence of a positive storm in the northern hemisphere. Overall, the strongest storm time disturbances were observed in the postsunset sector (~20:30–21:30 LT), where satellite radar altimeters TOPEX and Jason 1, along with the CHAMP satellite showed ~250–400% TEC increase in the middle‐ and low‐latitude regions. The signatures of the ionospheric plasma enhancement were seen up to the height of the Defense Meteorological Satellite Program (DMSP) satellites (~840 km). As for the thermospheric storm, data of the Gravity Recovery and Climate Experiment (GRACE) satellite mission revealed no asymmetry in neutral density data in the evening sector (~17 UT); however, very strong hemispheric asymmetry was observed in the postsunset sector by CHAMP (~21 UT). Overall, neutral density increase in the postsunset sector was found to be much stronger than in the evening sector. |
publishDate |
2014 |
dc.date.accessioned.none.fl_str_mv |
2018-11-19T09:54:06Z |
dc.date.available.none.fl_str_mv |
2018-11-19T09:54:06Z |
dc.date.issued.fl_str_mv |
2014-12-12 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
dc.identifier.citation.none.fl_str_mv |
Astafyeva, E., Zakharenkova, I., & Doornbos, E. (2014). Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004.==$Journal of Geophysical Research: Space Physics, 120$==(1), 697-714. https://doi.org/10.1002/2014JA020710 |
dc.identifier.uri.none.fl_str_mv |
http://hdl.handle.net/20.500.12816/3692 |
dc.identifier.journal.none.fl_str_mv |
Journal of Geophysical Research: Space Physics |
dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1002/2014JA020710 |
identifier_str_mv |
Astafyeva, E., Zakharenkova, I., & Doornbos, E. (2014). Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004.==$Journal of Geophysical Research: Space Physics, 120$==(1), 697-714. https://doi.org/10.1002/2014JA020710 Journal of Geophysical Research: Space Physics |
url |
http://hdl.handle.net/20.500.12816/3692 https://doi.org/10.1002/2014JA020710 |
dc.language.iso.none.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.none.fl_str_mv |
urn:issn:2169-9380 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
American Geophysical Union |
publisher.none.fl_str_mv |
American Geophysical Union |
dc.source.none.fl_str_mv |
reponame:IGP-Institucional instname:Instituto Geofísico del Perú instacron:IGP |
instname_str |
Instituto Geofísico del Perú |
instacron_str |
IGP |
institution |
IGP |
reponame_str |
IGP-Institucional |
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IGP-Institucional |
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Astafyeva, ElviraZakharenkova, IrinaDoornbos, Eelco2018-11-19T09:54:06Z2018-11-19T09:54:06Z2014-12-12Astafyeva, E., Zakharenkova, I., & Doornbos, E. (2014). Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004.==$Journal of Geophysical Research: Space Physics, 120$==(1), 697-714. https://doi.org/10.1002/2014JA020710http://hdl.handle.net/20.500.12816/3692Journal of Geophysical Research: Space Physicshttps://doi.org/10.1002/2014JA020710By making use of multiple ground‐based and spaceborne instruments, we study ionospheric and thermospheric behavior during the moderately intense geomagnetic storm of 29–31 August 2004 (minimum Dst excursion of −128 nT). Although this storm was far from the strongest in solar cycle 23, it provoked quite interesting effects in the ionosphere, such as opposite hemispheric asymmetries in the ionospheric F layer and in the topside ionosphere and a development of the ionospheric superfountain effect in the postsunset sector. Data from ground‐based GPS receivers and ionosondes revealed large increase in total electron content (TEC) and in NmF2 in the southern hemisphere, whereas in the northern hemisphere, very weak or no effect was observed. On the contrary, the topside measurements indicated the occurrence of a positive storm in the northern hemisphere. Overall, the strongest storm time disturbances were observed in the postsunset sector (~20:30–21:30 LT), where satellite radar altimeters TOPEX and Jason 1, along with the CHAMP satellite showed ~250–400% TEC increase in the middle‐ and low‐latitude regions. The signatures of the ionospheric plasma enhancement were seen up to the height of the Defense Meteorological Satellite Program (DMSP) satellites (~840 km). As for the thermospheric storm, data of the Gravity Recovery and Climate Experiment (GRACE) satellite mission revealed no asymmetry in neutral density data in the evening sector (~17 UT); however, very strong hemispheric asymmetry was observed in the postsunset sector by CHAMP (~21 UT). Overall, neutral density increase in the postsunset sector was found to be much stronger than in the evening sector.Por paresapplication/pdfengAmerican Geophysical Unionurn:issn:2169-9380info:eu-repo/semantics/openAccessIonospheric stormHemispheric asymmetryTopside contributionSuperfountain effectThermospheric stormPostsunset sectorhttp://purl.org/pe-repo/ocde/ford#1.05.01Opposite hemispheric asymmetries during the ionospheric storm of 29-31 August 2004info:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALIGP-1-1-1-1495143938.pdfIGP-1-1-1-1495143938.pdfapplication/pdf2524783https://repositorio.igp.gob.pe/bitstreams/6b7dcee3-fc96-49bf-9fa7-0b5438a19481/download388fcaeb4027b5edeb78c93b0a51b223MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-8391https://repositorio.igp.gob.pe/bitstreams/7f7418ab-39ff-48fe-80ae-851e4cf4e11f/downloadef941c35636116525aadeaab7bbf4ca3MD52THUMBNAILIGP-1-1-1-1495143938.pdf.jpgIGP-1-1-1-1495143938.pdf.jpgIM Thumbnailimage/jpeg107712https://repositorio.igp.gob.pe/bitstreams/5fa30a84-a87d-4dca-a573-8e8864b74f8a/download24f86273725868ad2605e14603224ddfMD53TEXTIGP-1-1-1-1495143938.pdf.txtIGP-1-1-1-1495143938.pdf.txtExtracted texttext/plain77913https://repositorio.igp.gob.pe/bitstreams/f24c76b9-cfd8-414d-81fd-8fa28515c77b/download7a07b7b8b6dd76f21684f56b3b7e28bfMD5420.500.12816/3692oai:repositorio.igp.gob.pe:20.500.12816/36922025-08-18 10:32:00.746open.accesshttps://repositorio.igp.gob.peRepositorio Geofísico Nacionalbiblio@igp.gob.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 |
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