2020
DOI: 10.1109/access.2020.3034347
|View full text |Cite
|
Sign up to set email alerts
|

A Review of Geomagnetically Induced Current Effects on Electrical Power System: Principles and Theory

Abstract: Geomagnetically induced current (GIC) has been a significant concern for the electrical power grid in high latitudes for decades. Its origin starts in the Sun; during extreme space weather, the magnetic field of the Earth varies rapidly. This variation induces electric fields at the Earth's surface and leads to GICs in manmade technologies. Power systems are the most affected by this induced current, which causes halfcycle saturation of power transformers and other issues. Understanding the behaviours and chai… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
7
0

Year Published

2021
2021
2023
2023

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 30 publications
(7 citation statements)
references
References 176 publications
(282 reference statements)
0
7
0
Order By: Relevance
“…At the surface, these geoelectric fields can drive GICs along power transmission lines and through grounded transformers, which can cause half‐cycle saturation. This distorts alternating‐current waveforms and can trip system relays, precipitating power‐system voltage collapse and heating, and, even, damage transformers (e.g., Abda et al., 2020; Kappenman, 2001; Molinski, 2002; Oyedokun and Cilliers, 2018; Samuelsson, 2013). Quantitative modeling of this convoluted chain of causes and effects, encompassing natural hazards and engineered systems, is an important objective of ongoing research and development (e.g., Gaunt, 2016; Pennington et al., 2021; Pilipenko, 2021; Pulkkinen et al., 2017; Thomson et al., 2010).…”
Section: Introductionmentioning
confidence: 99%
“…At the surface, these geoelectric fields can drive GICs along power transmission lines and through grounded transformers, which can cause half‐cycle saturation. This distorts alternating‐current waveforms and can trip system relays, precipitating power‐system voltage collapse and heating, and, even, damage transformers (e.g., Abda et al., 2020; Kappenman, 2001; Molinski, 2002; Oyedokun and Cilliers, 2018; Samuelsson, 2013). Quantitative modeling of this convoluted chain of causes and effects, encompassing natural hazards and engineered systems, is an important objective of ongoing research and development (e.g., Gaunt, 2016; Pennington et al., 2021; Pilipenko, 2021; Pulkkinen et al., 2017; Thomson et al., 2010).…”
Section: Introductionmentioning
confidence: 99%
“…One well‐known and important space weather effect detected on the ground is manifested as the so‐called geomagnetically induced currents (GICs). Sharp variations of the surface geomagnetic field (d B /d t ) generate geoelectric fields, which in turn couple with artificial conductors giving rise to the flow of undesirable GICs (Abda et al., 2020; Belakhovsky et al., 2019; Oliveira & Ngwira, 2017; Viljanen, 1998). Although ground conductivity models are necessary to compute geoelectric fields that generate GICs (Liu et al., 2019; Love et al., 2016), d B /d t variations are an acceptable and widely used proxy for assessing GIC response to space weather because such geoelectric fields may exist independent of ground artificial conductors.…”
Section: Introductionmentioning
confidence: 99%
“…There are various methods for calculating the geoelectric field [E] (see details in, e.g., Abda et al, 2020, and the references therein). In the frame work of this article, we estimated E from one-minute geomagnetic field data [B] in the frequency domain using a 1D layered conductivity Earth model (Boteler, Pirjola, and Marti, 2019;.…”
Section: Geoelectric Field Computationmentioning
confidence: 99%
“…This model considers the change of conductivity with depth. More precisely, the Earth is represented by N horizontal layers, which are assumed to be homogeneous and infinitely extended in the X (northward) and Y (eastward) directions (Abda et al, 2020). In the Z (downward) direction, each layer is specified by conductivity σ n and thickness l n (n = 1, .…”
Section: Geoelectric Field Computationmentioning
confidence: 99%