Swarm equatorial electric field chain: First results

Descripción del Articulo

The eastward equatorial electric field (EEF) in the E region ionosphere drives many important phenomena at low latitudes. We developed a method of estimating the EEF from magnetometer measurements of near‐polar orbiting satellites as they cross the magnetic equator, by recovering a clean signal of t...

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Detalles Bibliográficos
Autores: Alken, P., Maus, S., Chulliat, A., Vigneron, P., Sirol, O., Hulot, G.
Formato: artículo
Fecha de Publicación:2015
Institución:Instituto Geofísico del Perú
Repositorio:IGP-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.igp.gob.pe:20.500.12816/3609
Enlace del recurso:http://hdl.handle.net/20.500.12816/3609
https://doi.org/10.1002/2014GL062658
Nivel de acceso:acceso abierto
Materia:Swarm
Ionosphere
Electrojet
Electric field
EEF
http://purl.org/pe-repo/ocde/ford#1.05.01
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spelling Alken, P.Maus, S.Chulliat, A.Vigneron, P.Sirol, O.Hulot, G.2018-11-14T17:35:27Z2018-11-14T17:35:27Z2015-01-13Alken, P., Maus, S., Chulliat, A., Vigneron, P., Sirol, O., & Hulot, G. (2015). Swarm equatorial electric field chain: First results.==$Geophysical Research Letters, 42$==(3), 673-680. https://doi.org/10.1002/2014GL062658http://hdl.handle.net/20.500.12816/3609Geophysical Research Lettershttps://doi.org/10.1002/2014GL062658The eastward equatorial electric field (EEF) in the E region ionosphere drives many important phenomena at low latitudes. We developed a method of estimating the EEF from magnetometer measurements of near‐polar orbiting satellites as they cross the magnetic equator, by recovering a clean signal of the equatorial electrojet current and modeling the observed current to determine the electric field present during the satellite pass. This algorithm is now implemented as an official Level‐2 Swarm product. Here we present first results of EEF estimates from nearly a year of Swarm data. We find excellent agreement with independent measurements from the ground‐based coherent scatter radar at Jicamarca, Peru, as well as horizontal field measurements from the West African Magnetometer Network magnetic observatory chain. We also calculate longitudinal gradients of EEF measurements made by the A and C lower satellite pair and find gradients up to about 0.05 mV/m/deg with significant longitudinal variability.Por paresapplication/pdfengAmerican Geophysical Unionurn:issn:0094-8276info:eu-repo/semantics/openAccessSwarmIonosphereElectrojetElectric fieldEEFhttp://purl.org/pe-repo/ocde/ford#1.05.01Swarm equatorial electric field chain: First resultsinfo:eu-repo/semantics/articlereponame:IGP-Institucionalinstname:Instituto Geofísico del Perúinstacron:IGPORIGINALIGP-1-1-1-1432154880.pdfIGP-1-1-1-1432154880.pdfapplication/pdf912995https://repositorio.igp.gob.pe/bitstreams/7023100a-8c91-449e-9be8-c620a21afff9/download7b38bda72609c371845c27b74b854533MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-8391https://repositorio.igp.gob.pe/bitstreams/fd49e3f0-0280-4404-8fb6-ba590889d793/downloadef941c35636116525aadeaab7bbf4ca3MD52THUMBNAILIGP-1-1-1-1432154880.pdf.jpgIGP-1-1-1-1432154880.pdf.jpgIM Thumbnailimage/jpeg103366https://repositorio.igp.gob.pe/bitstreams/c26eccf0-9dde-4d5a-bfb9-3efe924205d8/downloaddaa8afb59206c0bceba10ba61731a024MD53TEXTIGP-1-1-1-1432154880.pdf.txtIGP-1-1-1-1432154880.pdf.txtExtracted texttext/plain32156https://repositorio.igp.gob.pe/bitstreams/174ff22d-40bb-4930-ae5c-4f7872358185/downloadaf86be0463dd86b23494c940c90b8dacMD5420.500.12816/3609oai:repositorio.igp.gob.pe:20.500.12816/36092025-08-13 09:50:52.738open.accesshttps://repositorio.igp.gob.peRepositorio Geofísico Nacionalbiblio@igp.gob.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
dc.title.none.fl_str_mv Swarm equatorial electric field chain: First results
title Swarm equatorial electric field chain: First results
spellingShingle Swarm equatorial electric field chain: First results
Alken, P.
Swarm
Ionosphere
Electrojet
Electric field
EEF
http://purl.org/pe-repo/ocde/ford#1.05.01
title_short Swarm equatorial electric field chain: First results
title_full Swarm equatorial electric field chain: First results
title_fullStr Swarm equatorial electric field chain: First results
title_full_unstemmed Swarm equatorial electric field chain: First results
title_sort Swarm equatorial electric field chain: First results
author Alken, P.
author_facet Alken, P.
Maus, S.
Chulliat, A.
Vigneron, P.
Sirol, O.
Hulot, G.
author_role author
author2 Maus, S.
Chulliat, A.
Vigneron, P.
Sirol, O.
Hulot, G.
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Alken, P.
Maus, S.
Chulliat, A.
Vigneron, P.
Sirol, O.
Hulot, G.
dc.subject.none.fl_str_mv Swarm
Ionosphere
Electrojet
Electric field
EEF
topic Swarm
Ionosphere
Electrojet
Electric field
EEF
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 The eastward equatorial electric field (EEF) in the E region ionosphere drives many important phenomena at low latitudes. We developed a method of estimating the EEF from magnetometer measurements of near‐polar orbiting satellites as they cross the magnetic equator, by recovering a clean signal of the equatorial electrojet current and modeling the observed current to determine the electric field present during the satellite pass. This algorithm is now implemented as an official Level‐2 Swarm product. Here we present first results of EEF estimates from nearly a year of Swarm data. We find excellent agreement with independent measurements from the ground‐based coherent scatter radar at Jicamarca, Peru, as well as horizontal field measurements from the West African Magnetometer Network magnetic observatory chain. We also calculate longitudinal gradients of EEF measurements made by the A and C lower satellite pair and find gradients up to about 0.05 mV/m/deg with significant longitudinal variability.
publishDate 2015
dc.date.accessioned.none.fl_str_mv 2018-11-14T17:35:27Z
dc.date.available.none.fl_str_mv 2018-11-14T17:35:27Z
dc.date.issued.fl_str_mv 2015-01-13
dc.type.none.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.none.fl_str_mv Alken, P., Maus, S., Chulliat, A., Vigneron, P., Sirol, O., & Hulot, G. (2015). Swarm equatorial electric field chain: First results.==$Geophysical Research Letters, 42$==(3), 673-680. https://doi.org/10.1002/2014GL062658
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/20.500.12816/3609
dc.identifier.journal.none.fl_str_mv Geophysical Research Letters
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1002/2014GL062658
identifier_str_mv Alken, P., Maus, S., Chulliat, A., Vigneron, P., Sirol, O., & Hulot, G. (2015). Swarm equatorial electric field chain: First results.==$Geophysical Research Letters, 42$==(3), 673-680. https://doi.org/10.1002/2014GL062658
Geophysical Research Letters
url http://hdl.handle.net/20.500.12816/3609
https://doi.org/10.1002/2014GL062658
dc.language.iso.none.fl_str_mv eng
language eng
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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
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instacron:IGP
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