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-...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2023
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11850/632669 https://doi.org/10.3929/ethz-b-000632669 |
_version_ | 1828059220372619264 |
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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 |
op_collection_id | ftethz |
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 |