Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities

Abstract An increase in geomagnetically induced currents (GICs) is an inevitable result of geomagnetic field disturbances, and is harmful to the power grid, in particular, at high latitudes. At mid and low latitudes, the amplitude of the GICs is, in general, small, but large‐amplitude GICs are often...

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Main Authors: T. Zhang, Y. Ebihara
Format: Article
Language:English
Published: Wiley 2022-05-01
Series:Space Weather
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Online Access:https://doi.org/10.1029/2021SW002893
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author T. Zhang
Y. Ebihara
author_facet T. Zhang
Y. Ebihara
author_sort T. Zhang
collection DOAJ
description Abstract An increase in geomagnetically induced currents (GICs) is an inevitable result of geomagnetic field disturbances, and is harmful to the power grid, in particular, at high latitudes. At mid and low latitudes, the amplitude of the GICs is, in general, small, but large‐amplitude GICs are often observed during magnetic storms. It is of importance to understand major characteristics and extreme values of GICs at mid and low latitudes. For the geoelectric field disturbances ΔE observed at Kakioka (27.8° geomagnetic latitude) in Japan in 1996–2004, we performed superposed epoch analyses with respect to three types of geomagnetic disturbances: (a) storm sudden commencements (SSCs)/sudden impulses (SIs), (b) main phase of magnetic storms, and (c) bay disturbances. It is shown that the SSCs/SIs and the main phase of the magnetic storms are equally important for causing large‐amplitude disturbances of ΔE at Kakioka. GICs are thought to be amplified when the SIs and/or the bay disturbances occur during the magnetic storms. The maximum value of ΔE tends to be correlated with the maximum value of ΔH during the three types of events, where ΔH is the horizontal component of the geomagnetic field. Assuming that a quasi‐linear relationship between the maximum ΔE and the maximum ΔH is valid, we estimated GICs at three substations in Japan for an extreme SSCs/SIs, and the extreme magnetic storms. This scheme could be applicable to estimate roughly the GICs against extreme events, and to forecast the maximum GICs in a real‐time manner.
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spelling doaj-art-003bcc010e404b5ab553fd220edb843c2025-01-14T16:31:05ZengWileySpace Weather1542-73902022-05-01205n/an/a10.1029/2021SW002893Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic ActivitiesT. Zhang0Y. Ebihara1Research Institute for Sustainable Humanosphere Kyoto University Kyoto JapanResearch Institute for Sustainable Humanosphere Kyoto University Kyoto JapanAbstract An increase in geomagnetically induced currents (GICs) is an inevitable result of geomagnetic field disturbances, and is harmful to the power grid, in particular, at high latitudes. At mid and low latitudes, the amplitude of the GICs is, in general, small, but large‐amplitude GICs are often observed during magnetic storms. It is of importance to understand major characteristics and extreme values of GICs at mid and low latitudes. For the geoelectric field disturbances ΔE observed at Kakioka (27.8° geomagnetic latitude) in Japan in 1996–2004, we performed superposed epoch analyses with respect to three types of geomagnetic disturbances: (a) storm sudden commencements (SSCs)/sudden impulses (SIs), (b) main phase of magnetic storms, and (c) bay disturbances. It is shown that the SSCs/SIs and the main phase of the magnetic storms are equally important for causing large‐amplitude disturbances of ΔE at Kakioka. GICs are thought to be amplified when the SIs and/or the bay disturbances occur during the magnetic storms. The maximum value of ΔE tends to be correlated with the maximum value of ΔH during the three types of events, where ΔH is the horizontal component of the geomagnetic field. Assuming that a quasi‐linear relationship between the maximum ΔE and the maximum ΔH is valid, we estimated GICs at three substations in Japan for an extreme SSCs/SIs, and the extreme magnetic storms. This scheme could be applicable to estimate roughly the GICs against extreme events, and to forecast the maximum GICs in a real‐time manner.https://doi.org/10.1029/2021SW002893geoelectric fieldgeomagnetic disturbancesSSCs/SIsintense magnetic stormsbay disturbancesmagnetospheric current systems
spellingShingle T. Zhang
Y. Ebihara
Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
Space Weather
geoelectric field
geomagnetic disturbances
SSCs/SIs
intense magnetic storms
bay disturbances
magnetospheric current systems
title Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
title_full Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
title_fullStr Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
title_full_unstemmed Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
title_short Superposed Epoch Analyses of Geoelectric Field Disturbances in Japan in Response to Different Geomagnetic Activities
title_sort superposed epoch analyses of geoelectric field disturbances in japan in response to different geomagnetic activities
topic geoelectric field
geomagnetic disturbances
SSCs/SIs
intense magnetic storms
bay disturbances
magnetospheric current systems
url https://doi.org/10.1029/2021SW002893
work_keys_str_mv AT tzhang superposedepochanalysesofgeoelectricfielddisturbancesinjapaninresponsetodifferentgeomagneticactivities
AT yebihara superposedepochanalysesofgeoelectricfielddisturbancesinjapaninresponsetodifferentgeomagneticactivities