Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions

Detalhes bibliográficos
Autor(a) principal: Owens, M. J.
Data de Publicação: 2016
Outros Autores: Cliver, E., McCracken, K. G., Beer, J., Barnard, L., Lockwood, M., Rouillard, A., Passos, Dário, Riley, P., Usoskin, I., Wang, Y-M.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.1/9399
Resumo: We present two separate time series of the near-Earth heliospheric magnetic field strength (B) based on geomagnetic data and sunspot number (SSN). The geomagnetic-based B series from 1845 to 2013 is a weighted composite of two series that employ the interdiurnal variability index; this series is highly correlated with in situ spacecraft measurements of B (correlation coefficient, r=0.94; mean square error, MSE=0.16nT(2)). The SSN-based estimate of B, from 1750 to 2013, is a weighted composite of eight time series derived from two separate reconstruction methods applied to four different SSN time series, allowing determination of the uncertainty from both the underlying sunspot records and the B reconstruction methods. The SSN-based composite is highly correlated with direct spacecraft measurements of B and with the composite geomagnetic B time series from 1845 to 2013 (r=0.91; MSE=0.24nT(2)), demonstrating that B can accurately reconstructed by both geomagnetic and sunspot-based methods. The composite sunspot and geomagnetic B time series, with uncertainties, are provided as supporting information.
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spelling Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructionsWe present two separate time series of the near-Earth heliospheric magnetic field strength (B) based on geomagnetic data and sunspot number (SSN). The geomagnetic-based B series from 1845 to 2013 is a weighted composite of two series that employ the interdiurnal variability index; this series is highly correlated with in situ spacecraft measurements of B (correlation coefficient, r=0.94; mean square error, MSE=0.16nT(2)). The SSN-based estimate of B, from 1750 to 2013, is a weighted composite of eight time series derived from two separate reconstruction methods applied to four different SSN time series, allowing determination of the uncertainty from both the underlying sunspot records and the B reconstruction methods. The SSN-based composite is highly correlated with direct spacecraft measurements of B and with the composite geomagnetic B time series from 1845 to 2013 (r=0.91; MSE=0.24nT(2)), demonstrating that B can accurately reconstructed by both geomagnetic and sunspot-based methods. The composite sunspot and geomagnetic B time series, with uncertainties, are provided as supporting information.SapientiaOwens, M. J.Cliver, E.McCracken, K. G.Beer, J.Barnard, L.Lockwood, M.Rouillard, A.Passos, DárioRiley, P.Usoskin, I.Wang, Y-M.2017-04-07T15:56:23Z2016-072016-07-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.1/9399eng2169-938010.1002/2016JA022529info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-07-24T10:20:51Zoai:sapientia.ualg.pt:10400.1/9399Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:01:21.383158Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
title Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
spellingShingle Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
Owens, M. J.
title_short Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
title_full Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
title_fullStr Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
title_full_unstemmed Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
title_sort Near-Earth heliospheric magnetic field intensity since 1750: 1. Sunspot and geomagnetic reconstructions
author Owens, M. J.
author_facet Owens, M. J.
Cliver, E.
McCracken, K. G.
Beer, J.
Barnard, L.
Lockwood, M.
Rouillard, A.
Passos, Dário
Riley, P.
Usoskin, I.
Wang, Y-M.
author_role author
author2 Cliver, E.
McCracken, K. G.
Beer, J.
Barnard, L.
Lockwood, M.
Rouillard, A.
Passos, Dário
Riley, P.
Usoskin, I.
Wang, Y-M.
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Sapientia
dc.contributor.author.fl_str_mv Owens, M. J.
Cliver, E.
McCracken, K. G.
Beer, J.
Barnard, L.
Lockwood, M.
Rouillard, A.
Passos, Dário
Riley, P.
Usoskin, I.
Wang, Y-M.
description We present two separate time series of the near-Earth heliospheric magnetic field strength (B) based on geomagnetic data and sunspot number (SSN). The geomagnetic-based B series from 1845 to 2013 is a weighted composite of two series that employ the interdiurnal variability index; this series is highly correlated with in situ spacecraft measurements of B (correlation coefficient, r=0.94; mean square error, MSE=0.16nT(2)). The SSN-based estimate of B, from 1750 to 2013, is a weighted composite of eight time series derived from two separate reconstruction methods applied to four different SSN time series, allowing determination of the uncertainty from both the underlying sunspot records and the B reconstruction methods. The SSN-based composite is highly correlated with direct spacecraft measurements of B and with the composite geomagnetic B time series from 1845 to 2013 (r=0.91; MSE=0.24nT(2)), demonstrating that B can accurately reconstructed by both geomagnetic and sunspot-based methods. The composite sunspot and geomagnetic B time series, with uncertainties, are provided as supporting information.
publishDate 2016
dc.date.none.fl_str_mv 2016-07
2016-07-01T00:00:00Z
2017-04-07T15:56:23Z
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url http://hdl.handle.net/10400.1/9399
dc.language.iso.fl_str_mv eng
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10.1002/2016JA022529
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