Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm

In this study, we perform three-dimensional (3-D) ground electric field (GEF) modeling in Fennoscandia for three days of the Halloween geomagnetic storm (29–31 October 2003) using magnetic field data from the International Monitor for Auroral Geomagnetic Effects (IMAGE) magnetometer network and a 3-...

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Main Authors: Marshalko, Elena, Kruglyakov, Mikhail, id_orcid:0 000-0002-6709-692X, Kuvshinov, Alexey, Viljanen, Ari
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2023
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/632669
https://doi.org/10.3929/ethz-b-000632669
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author Marshalko, Elena
Kruglyakov, Mikhail
id_orcid:0 000-0002-6709-692X
Kuvshinov, Alexey
Viljanen, Ari
author_facet Marshalko, Elena
Kruglyakov, Mikhail
id_orcid:0 000-0002-6709-692X
Kuvshinov, Alexey
Viljanen, Ari
author_sort Marshalko, Elena
collection ETH Zürich Research Collection
description In this study, we perform three-dimensional (3-D) ground electric field (GEF) modeling in Fennoscandia for three days of the Halloween geomagnetic storm (29–31 October 2003) using magnetic field data from the International Monitor for Auroral Geomagnetic Effects (IMAGE) magnetometer network and a 3-D conductivity model of the region. To explore the influence of the inducing source model on 3-D GEF simulations, we consider three different approaches to source approximation. Within the first two approaches, the source varies laterally, whereas in the third method, the GEF is calculated by implementing the time-domain realization of the magnetotelluric intersite impedance method. We then compare GEF-based geomagnetically induced current (GIC) with observations at the Mäntsälä natural gas pipeline recording point. We conclude that a high correlation between modeled and recorded GIC is observed for all considered approaches. The highest correlation is achieved when performing a 3-D GEF simulation using a “conductivity-based” laterally nonuniform inducing source. Our results also highlight the strong dependence of the GEF on the earth's conductivity distribution. ISSN:1542-7390
format Article in Journal/Newspaper
genre Fennoscandia
genre_facet Fennoscandia
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/632669
institution Open Polar
language English
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op_doi https://doi.org/20.500.11850/63266910.3929/ethz-b-00063266910.1029/2022SW003370
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2022SW003370
info:eu-repo/semantics/altIdentifier/wos/001067956700001
http://hdl.handle.net/20.500.11850/632669
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_source Space Weather, 21 (9)
publishDate 2023
publisher American Geophysical Union
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/632669 2025-03-30T15:11:16+00:00 Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm Marshalko, Elena Kruglyakov, Mikhail id_orcid:0 000-0002-6709-692X Kuvshinov, Alexey Viljanen, Ari 2023-09 application/application/pdf https://hdl.handle.net/20.500.11850/632669 https://doi.org/10.3929/ethz-b-000632669 en eng American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2022SW003370 info:eu-repo/semantics/altIdentifier/wos/001067956700001 http://hdl.handle.net/20.500.11850/632669 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Space Weather, 21 (9) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2023 ftethz https://doi.org/20.500.11850/63266910.3929/ethz-b-00063266910.1029/2022SW003370 2025-03-05T22:09:17Z In this study, we perform three-dimensional (3-D) ground electric field (GEF) modeling in Fennoscandia for three days of the Halloween geomagnetic storm (29–31 October 2003) using magnetic field data from the International Monitor for Auroral Geomagnetic Effects (IMAGE) magnetometer network and a 3-D conductivity model of the region. To explore the influence of the inducing source model on 3-D GEF simulations, we consider three different approaches to source approximation. Within the first two approaches, the source varies laterally, whereas in the third method, the GEF is calculated by implementing the time-domain realization of the magnetotelluric intersite impedance method. We then compare GEF-based geomagnetically induced current (GIC) with observations at the Mäntsälä natural gas pipeline recording point. We conclude that a high correlation between modeled and recorded GIC is observed for all considered approaches. The highest correlation is achieved when performing a 3-D GEF simulation using a “conductivity-based” laterally nonuniform inducing source. Our results also highlight the strong dependence of the GEF on the earth's conductivity distribution. ISSN:1542-7390 Article in Journal/Newspaper Fennoscandia ETH Zürich Research Collection
spellingShingle Marshalko, Elena
Kruglyakov, Mikhail
id_orcid:0 000-0002-6709-692X
Kuvshinov, Alexey
Viljanen, Ari
Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title_full Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title_fullStr Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title_full_unstemmed Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title_short Three-Dimensional Modeling of the Ground Electric Field in Fennoscandia During the Halloween Geomagnetic Storm
title_sort three-dimensional modeling of the ground electric field in fennoscandia during the halloween geomagnetic storm
url https://hdl.handle.net/20.500.11850/632669
https://doi.org/10.3929/ethz-b-000632669