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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/3T3HSMP
Repositorysid.inpe.br/mtc-m21c/2019/04.02.16.38   (restricted access)
Last Update2019:04.02.16.38.34 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2019/04.02.16.38.34
Metadata Last Update2022:03.18.22.11.29 (UTC) administrator
DOI10.1029/2018SW002094
ISSN1542-7390
Citation KeyEspinosaSarmientoPadiAlve:2019:CaStLo
TitleEffects of ionospheric conductivity and ground conductance on geomagnetically induced currents during geomagnetic storms: case studies at low-latitude and Equatorial regions
Year2019
MonthFeb.
Access Date2024, May 17
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size3553 KiB
2. Context
Author1 Espinosa Sarmiento, Karen Viviana
2 Padilha, Antonio Lopes
3 Alves, Livia Ribeiro
Resume Identifier1
2 8JMKD3MGP5W/3C9JGJG
Group1 GESAST-CEA-SESPG-INPE-MCTIC-GOV-BR
2 DIDGE-CGCEA-INPE-MCTIC-GOV-BR
3 DIDGE-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 karen.sarmiento@inpe.br
2 antonio.padilha@inpe.br
3 livia.alves@inpe.br
JournalSpace Weather
Volume17
Number2
Pages252-268
Secondary MarkB1_INTERDISCIPLINAR B1_GEOCIÊNCIAS B2_ASTRONOMIA_/_FÍSICA
History (UTC)2019-04-02 16:38:44 :: simone -> administrator :: 2019
2022-03-18 22:11:29 :: administrator -> simone :: 2019
3. Content and structure
Is the master or a copy?is the master
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Transferable1
Content TypeExternal Contribution
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AbstractGeomagnetic field variations recorded by fluxgate magnetometers are used to evaluate geomagnetically induced currents (GICs) under the equatorial electrojet (EEJ) and South Atlantic Magnetic Anomaly (SAMA) during two geomagnetic storms in March and June 2015. Geomagnetic stations with information about the underground electrical conductivity structure and that can be approximated by unidimensional (1-D) models for calculation of the geoelectric field are selected. GICs levels are estimated using a realistic local power grid model located in the central region of Brazil, artificially moved to the sites where the geomagnetic measurements are available. GIC magnitudes are not large during the storms, and a maximum amplitude of 3.8 A was estimated at an equatorial station positioned over high resistivity underground during the main phase of the June storm. Effects of the ionospheric currents over the measurement sites and of the conductivity distribution beneath these sites are also evaluated. It is observed that both (EEJ) and (SAMA) increase the GICs amplitudes, with the greatest effects associated with daytime (EEJ) currents. A cutoff frequency was identified for both the (EEJ) and (SAMA) so that signals with frequencies lower than 2 mHz (periods longer than 500 s) are not amplified by the ionospheric currents. In relation to the underlying conductivity structure, GIC magnitude is affected by variation of the surface impedance and the sampling rate of the geomagnetic field. In our case, differences in amplitude of the surface impedance at the Nyquist frequency control the relative effects of the ground conductance between the stations.
AreaCEA
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4. Conditions of access and use
Languageen
Target FileEspinosa_et_al-2019-Space_Weather.pdf
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Visibilityshown
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/3F2PBEE
Citing Item Listsid.inpe.br/bibdigital/2013/10.01.22.11 4
sid.inpe.br/mtc-m21/2012/07.13.14.40.26 2
DisseminationWEBSCI; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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