Estimating Extreme Geoelectric Field Values for the Australian Region

Abstract There are a number of global initiatives to understand and mitigate the impacts of extreme space weather on critical infrastructure and modern society. This paper provides the results of an analysis to estimate extreme geoelectric field values for the Australian region to facilitate evaluat...

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Main Authors: Richard Marshall, Léna Dziura, Liejun Wang, Jeanne Young, Michael Terkildsen
Format: Article
Language:English
Published: Wiley 2020-11-01
Series:Space Weather
Subjects:
Online Access:https://doi.org/10.1029/2020SW002512
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author Richard Marshall
Léna Dziura
Liejun Wang
Jeanne Young
Michael Terkildsen
author_facet Richard Marshall
Léna Dziura
Liejun Wang
Jeanne Young
Michael Terkildsen
author_sort Richard Marshall
collection DOAJ
description Abstract There are a number of global initiatives to understand and mitigate the impacts of extreme space weather on critical infrastructure and modern society. This paper provides the results of an analysis to estimate extreme geoelectric field values for the Australian region to facilitate evaluation of Australia's power system response to extreme geomagnetic storms. Geoelectric fields are calculated using a grid of modeled magnetotelluric impedance tensors obtained from a 3‐D conductivity model of the Australian region. Statistical metrics derived from grids of geoelectric field time series are analyzed as a function of Dst index for different storm days to extrapolate geoelectric fields to extreme storm levels over a range of ground conductivity conditions. For Carrington event storm levels, geoelectric field values of 5.3 ± 3.8 V/km in the north‐south direction and 9.6 ± 4.3 V/km in the east‐west direction are expected for areas of electrically resistive rocks near coastlines that are adjacent to deep highly conductive oceans, and inland, where there are large contrasts between the electrical conductivities of different rock types across Australia. Further, geoelectric field values may change by at least an order of magnitude over the grid spacing interval of 50 km in these areas. The results of the analysis also suggest that upscaling grids of geoelectric field time series derived from an observed storm by the ratio of extreme storm Dst to the observed storm Dst are a valid approach for the Australian region that provides extreme storm scenarios for different storm morphologies.
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institution Kabale University
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publishDate 2020-11-01
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spelling doaj-art-932b059719af4da9885b70a3f340041b2025-01-14T16:30:47ZengWileySpace Weather1542-73902020-11-011811n/an/a10.1029/2020SW002512Estimating Extreme Geoelectric Field Values for the Australian RegionRichard Marshall0Léna Dziura1Liejun Wang2Jeanne Young3Michael Terkildsen4Space Weather Services Bureau of Meteorology Melbourne Victoria AustraliaSpace Weather Services Bureau of Meteorology Melbourne Victoria AustraliaGeoscience Australia Canberra AustraliaSpace Weather Services Bureau of Meteorology Melbourne Victoria AustraliaSpace Weather Services Bureau of Meteorology Melbourne Victoria AustraliaAbstract There are a number of global initiatives to understand and mitigate the impacts of extreme space weather on critical infrastructure and modern society. This paper provides the results of an analysis to estimate extreme geoelectric field values for the Australian region to facilitate evaluation of Australia's power system response to extreme geomagnetic storms. Geoelectric fields are calculated using a grid of modeled magnetotelluric impedance tensors obtained from a 3‐D conductivity model of the Australian region. Statistical metrics derived from grids of geoelectric field time series are analyzed as a function of Dst index for different storm days to extrapolate geoelectric fields to extreme storm levels over a range of ground conductivity conditions. For Carrington event storm levels, geoelectric field values of 5.3 ± 3.8 V/km in the north‐south direction and 9.6 ± 4.3 V/km in the east‐west direction are expected for areas of electrically resistive rocks near coastlines that are adjacent to deep highly conductive oceans, and inland, where there are large contrasts between the electrical conductivities of different rock types across Australia. Further, geoelectric field values may change by at least an order of magnitude over the grid spacing interval of 50 km in these areas. The results of the analysis also suggest that upscaling grids of geoelectric field time series derived from an observed storm by the ratio of extreme storm Dst to the observed storm Dst are a valid approach for the Australian region that provides extreme storm scenarios for different storm morphologies.https://doi.org/10.1029/2020SW002512extreme geoelectric fieldmagnetotelluricsgeomagnetically induced current
spellingShingle Richard Marshall
Léna Dziura
Liejun Wang
Jeanne Young
Michael Terkildsen
Estimating Extreme Geoelectric Field Values for the Australian Region
Space Weather
extreme geoelectric field
magnetotellurics
geomagnetically induced current
title Estimating Extreme Geoelectric Field Values for the Australian Region
title_full Estimating Extreme Geoelectric Field Values for the Australian Region
title_fullStr Estimating Extreme Geoelectric Field Values for the Australian Region
title_full_unstemmed Estimating Extreme Geoelectric Field Values for the Australian Region
title_short Estimating Extreme Geoelectric Field Values for the Australian Region
title_sort estimating extreme geoelectric field values for the australian region
topic extreme geoelectric field
magnetotellurics
geomagnetically induced current
url https://doi.org/10.1029/2020SW002512
work_keys_str_mv AT richardmarshall estimatingextremegeoelectricfieldvaluesfortheaustralianregion
AT lenadziura estimatingextremegeoelectricfieldvaluesfortheaustralianregion
AT liejunwang estimatingextremegeoelectricfieldvaluesfortheaustralianregion
AT jeanneyoung estimatingextremegeoelectricfieldvaluesfortheaustralianregion
AT michaelterkildsen estimatingextremegeoelectricfieldvaluesfortheaustralianregion