2013
DOI: 10.1002/swe.20073
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Surface electric fields for North America during historical geomagnetic storms

Abstract: [1] To better understand the impact of geomagnetic disturbances on the electric grid, we recreate surface electric fields from two historical geomagnetic storms-the 1989 "Quebec" storm and the 2003 "Halloween" storms. Using the Spherical Elementary Current Systems method, we interpolate sparsely distributed magnetometer data across North America. We find good agreement between the measured and interpolated data, with larger RMS deviations at higher latitudes corresponding to larger magnetic field variations. T… Show more

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Cited by 60 publications
(60 citation statements)
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“…For comparison, Langlois et al (1996) reports the maximum measured value of 1.7 V/km in Québec, Canada, within a 500-day period, in an area that corresponds to South Finland in geomagnetic latitudes. Model calculations in North America by Wei et al (2013) and Nikitina et al (2016) indicate values up to 2-5 V/km. We remind that the electric field is very sensitive to the conductivity, so different ground models can produce fields with clearly different magnitudes when the same magnetic field is used as input.…”
Section: Methodsmentioning
confidence: 96%
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“…For comparison, Langlois et al (1996) reports the maximum measured value of 1.7 V/km in Québec, Canada, within a 500-day period, in an area that corresponds to South Finland in geomagnetic latitudes. Model calculations in North America by Wei et al (2013) and Nikitina et al (2016) indicate values up to 2-5 V/km. We remind that the electric field is very sensitive to the conductivity, so different ground models can produce fields with clearly different magnitudes when the same magnetic field is used as input.…”
Section: Methodsmentioning
confidence: 96%
“…The geoelectric field varies rapidly temporarily and spatially as demonstrated, for example, by Beggan et al (2013), Bedrosian and Love (2015), Wei et al (2013) and Wang et al (2016) for regional and continental scales, and by Püthe and Kuvshinov (2013) and Ngwira et al (2015) for global scales. Temporal variations are due to time variations of space currents and are connected with time variations of the geomagnetic field by Faraday's law.…”
Section: Introductionmentioning
confidence: 99%
“…They usually increase with geomagnetic latitude, transmission line length and voltage, but decrease with distance to the ocean and increased ground resistivity (Wei et al, 2013). Space-weather events also cause auroras, usually in two small ovals around 65 (±5) degrees northern and southern latitude that vary in size, location and intensity during geomagnetic storms.…”
Section: Introductionmentioning
confidence: 99%
“…These frequencies are comparable to other severe natural disasters, such as large earthquakes and volcanic eruptions. Power grids typically experience problems when the rate of change of the magnetic field exceeds a 100-200 nT min −1 (Wei et al, 2013). Occurring today, the Quebec 1989 event or the 1859 Carrington event would have a profound impact on the daily lives of millions of people, both through direct effects and via the impacts to the globalized economic production system.…”
Section: Introductionmentioning
confidence: 99%
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