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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/49453P8
Repositorysid.inpe.br/mtc-m21d/2023/05.09.14.16   (restricted access)
Last Update2023:05.09.14.16.03 (UTC) self-uploading-INPE-MCTI-GOV-BR
Metadata Repositorysid.inpe.br/mtc-m21d/2023/05.09.14.16.03
Metadata Last Update2024:01.02.17.16.43 (UTC) administrator
DOI10.1029/2022SW003166
ISSN1542-7390
Labelself-archiving-INPE-MCTIC-GOV-BR
Citation KeyEspinosaSarmientoPadAlvSchKel:2023:EsGeIn
TitleEstimating geomagnetically induced currents in southern Brazil using 3-D Earth resistivity model
Year2023
MonthApr.
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size4050 KiB
2. Context
Author1 Espinosa Sarmiento, Karen Viviana
2 Padilha, Antonio Lopes
3 Alves, Livia Ribeiro
4 Schultz, Adam
5 Kelbert, Anna
Resume Identifier1
2 8JMKD3MGP5W/3C9JGJG
ORCID1 0000-0001-5215-1132
2
3 0000-0002-5680-7271
4 0000-0003-1663-1547
5 0000-0003-4395-398X
Group1 GESAST-CEA-DIPGR-INPE-MCTI-GOV-BR
2 DIHPA-CGCE-INPE-MCTI-GOV-BR
3 DIHPA-CGCE-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Oregon State University
5 U.S. Geological Survey
Author e-Mail Address1 karen.sarmiento@inpe.br
2
3 livia.alves@inpe.br
JournalSpace Weather
Volume21
Number4
Pagese2022SW003166
Secondary MarkB1_INTERDISCIPLINAR B1_GEOCIÊNCIAS B2_ASTRONOMIA_/_FÍSICA
History (UTC)2023-05-09 14:16:31 :: simone -> administrator :: 2023
2023-12-18 23:44:32 :: administrator -> self-uploading-INPE-MCTI-GOV-BR :: 2023
2023-12-19 02:40:36 :: self-uploading-INPE-MCTI-GOV-BR -> administrator :: 2023
2024-01-02 17:16:43 :: administrator -> simone :: 2023
3. Content and structure
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Content TypeExternal Contribution
Version Typepublisher
AbstractGeomagnetically induced currents (GICs) result from the interaction of the time variation of ground magnetic field during a geomagnetic disturbance with the Earth's deep electrical resistivity structure. In this study, we simulate induced GICs in a hypothetical representation of a low-latitude power transmission network located mainly over the large Paleozoic Paraná basin (PB) in southern Brazil. Two intense geomagnetic storms in June and December 2015 are chosen and geoelectric fields are calculated by convolving a three-dimensional (3-D) Earth resistivity model with recorded geomagnetic variations. The dB/dt proxy often used to characterize GIC activity fails during the June storm mainly due to the relationship of the instantaneous geoelectric field to previous magnetic field values. Precise resistances of network components are unknown, so assumptions are made for calculating GIC flows from the derived geoelectric field. The largest GICs are modeled in regions of low conductance in the 3-D resistivity model, concentrated in an isolated substation at the northern edge of the network and in a cluster of substations in its central part where the east-west (E-W) oriented transmission lines coincide with the orientation of the instantaneous geoelectric field. The maximum magnitude of the modeled GIC was obtained during the main phase of the June storm, modeled at a northern substation, while the lowest magnitudes were found over prominent crustal anomalies along the PB axis and bordering the continental margin. The simulation results will be used to prospect the optimal substations for installation of GIC monitoring equipment.
AreaCEA
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4. Conditions of access and use
Languageen
Target FileSpace Weather - 2023 - Espinosa - Estimating Geomagnetically Induced Currents in Southern Brazil Using 3‐D Earth.pdf
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Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3F2PBEE
8JMKD3MGPCW/46KTFK8
DisseminationWEBSCI; SCOPUS.
Host Collectionurlib.net/www/2021/06.04.03.40
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