On the Regional Variability of dB/dt and Its Significance to GIC

Abstract Faraday's law of induction is responsible for setting up a geoelectric field due to the variations in the geomagnetic field caused by ionospheric currents. This drives geomagnetically induced currents (GICs) which flow in large ground‐based technological infrastructure such as high‐vol...

Full description

Saved in:
Bibliographic Details
Main Authors: A. P. Dimmock, L. Rosenqvist, D. T. Welling, A. Viljanen, I. Honkonen, R. J. Boynton, E. Yordanova
Format: Article
Language:English
Published: Wiley 2020-08-01
Series:Space Weather
Subjects:
Online Access:https://doi.org/10.1029/2020SW002497
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1841536470324609024
author A. P. Dimmock
L. Rosenqvist
D. T. Welling
A. Viljanen
I. Honkonen
R. J. Boynton
E. Yordanova
author_facet A. P. Dimmock
L. Rosenqvist
D. T. Welling
A. Viljanen
I. Honkonen
R. J. Boynton
E. Yordanova
author_sort A. P. Dimmock
collection DOAJ
description Abstract Faraday's law of induction is responsible for setting up a geoelectric field due to the variations in the geomagnetic field caused by ionospheric currents. This drives geomagnetically induced currents (GICs) which flow in large ground‐based technological infrastructure such as high‐voltage power lines. The geoelectric field is often a localized phenomenon exhibiting significant variations over spatial scales of only hundreds of kilometers. This is due to the complex spatiotemporal behavior of electrical currents flowing in the ionosphere and/or large gradients in the ground conductivity due to highly structured local geological properties. Over some regions, and during large storms, both of these effects become significant. In this study, we quantify the regional variability of dB/dt using closely placed IMAGE stations in northern Fennoscandia. The dependency between regional variability, solar wind conditions, and geomagnetic indices are also investigated. Finally, we assess the significance of spatial geomagnetic variations to modeling GICs across a transmission line. Key results from this study are as follows: (1) Regional geomagnetic disturbances are important in modeling GIC during strong storms; (2) dB/dt can vary by several times up to a factor of three compared to the spatial average; (3) dB/dt and its regional variation is coupled to the energy deposited into the magnetosphere; and (4) regional variability can be more accurately captured and predicted from a local index as opposed to a global one. These results demonstrate the need for denser magnetometer networks at high latitudes where transmission lines extending hundreds of kilometers are present.
format Article
id doaj-art-343eed10ffa64e4b80395cb697081d2c
institution Kabale University
issn 1542-7390
language English
publishDate 2020-08-01
publisher Wiley
record_format Article
series Space Weather
spelling doaj-art-343eed10ffa64e4b80395cb697081d2c2025-01-14T16:27:11ZengWileySpace Weather1542-73902020-08-01188n/an/a10.1029/2020SW002497On the Regional Variability of dB/dt and Its Significance to GICA. P. Dimmock0L. Rosenqvist1D. T. Welling2A. Viljanen3I. Honkonen4R. J. Boynton5E. Yordanova6Swedish Institute of Space Physics Uppsala SwedenSwedish Research Defence Agency Stockholm SwedenDepartment of Physics University of Texas at Arlington Arlington TX USAFinnish Meteorological Institute Helsinki FinlandFinnish Meteorological Institute Helsinki FinlandDepartment of Automatic Control and Systems Engineering University of Sheffield Sheffield UKSwedish Institute of Space Physics Uppsala SwedenAbstract Faraday's law of induction is responsible for setting up a geoelectric field due to the variations in the geomagnetic field caused by ionospheric currents. This drives geomagnetically induced currents (GICs) which flow in large ground‐based technological infrastructure such as high‐voltage power lines. The geoelectric field is often a localized phenomenon exhibiting significant variations over spatial scales of only hundreds of kilometers. This is due to the complex spatiotemporal behavior of electrical currents flowing in the ionosphere and/or large gradients in the ground conductivity due to highly structured local geological properties. Over some regions, and during large storms, both of these effects become significant. In this study, we quantify the regional variability of dB/dt using closely placed IMAGE stations in northern Fennoscandia. The dependency between regional variability, solar wind conditions, and geomagnetic indices are also investigated. Finally, we assess the significance of spatial geomagnetic variations to modeling GICs across a transmission line. Key results from this study are as follows: (1) Regional geomagnetic disturbances are important in modeling GIC during strong storms; (2) dB/dt can vary by several times up to a factor of three compared to the spatial average; (3) dB/dt and its regional variation is coupled to the energy deposited into the magnetosphere; and (4) regional variability can be more accurately captured and predicted from a local index as opposed to a global one. These results demonstrate the need for denser magnetometer networks at high latitudes where transmission lines extending hundreds of kilometers are present.https://doi.org/10.1029/2020SW002497space weatherGICpower gridmagnetic stormsgeoelectric fieldground conductivity
spellingShingle A. P. Dimmock
L. Rosenqvist
D. T. Welling
A. Viljanen
I. Honkonen
R. J. Boynton
E. Yordanova
On the Regional Variability of dB/dt and Its Significance to GIC
Space Weather
space weather
GIC
power grid
magnetic storms
geoelectric field
ground conductivity
title On the Regional Variability of dB/dt and Its Significance to GIC
title_full On the Regional Variability of dB/dt and Its Significance to GIC
title_fullStr On the Regional Variability of dB/dt and Its Significance to GIC
title_full_unstemmed On the Regional Variability of dB/dt and Its Significance to GIC
title_short On the Regional Variability of dB/dt and Its Significance to GIC
title_sort on the regional variability of db dt and its significance to gic
topic space weather
GIC
power grid
magnetic storms
geoelectric field
ground conductivity
url https://doi.org/10.1029/2020SW002497
work_keys_str_mv AT apdimmock ontheregionalvariabilityofdbdtanditssignificancetogic
AT lrosenqvist ontheregionalvariabilityofdbdtanditssignificancetogic
AT dtwelling ontheregionalvariabilityofdbdtanditssignificancetogic
AT aviljanen ontheregionalvariabilityofdbdtanditssignificancetogic
AT ihonkonen ontheregionalvariabilityofdbdtanditssignificancetogic
AT rjboynton ontheregionalvariabilityofdbdtanditssignificancetogic
AT eyordanova ontheregionalvariabilityofdbdtanditssignificancetogic