What is it about?

In support of a multiagency project for assessing induction hazards, we present maps ofextreme-value geoelectric amplitudes over about half of the continental United States. These mapsare constructed using a parameterization of induction: estimates of Earth surface impedance, obtainedat discrete geographic sites from magnetotelluric survey data, are convolved with latitude-dependentstatistical maps of extreme-value geomagnetic activity, obtained from decades of magnetic observatorydata. Geoelectric amplitudes are estimated for geomagnetic waveforms having 240 s sinusoidal periodand amplitudes over 10 min that exceed a once-per-century threshold. As a result of the combination ofgeographic differences in geomagnetic activity and Earth surface impedance, once-per-century geoelectricamplitudes span more than 2 orders of magnitude and are an intricate function of location. For north-southinduction, once-per-century geoelectric amplitudes across large parts of the United States have a medianvalue of 0.26 V/km; for east-west geomagnetic variation the median value is 0.23 V/km. At some locations,once-per-century geoelectric amplitudes exceed 3 V/km.

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Why is it important?

This work provides realistic estimates of geoelectric hazards that can interfere with the operation of electric-power grid systems.

Perspectives

This work is motivated by priorities set by the Space Weather Operations Response and Mitigation (SWORM) Subcommittee of the United States National Science and Technology Council.

Dr Jeffrey Love
Geomagnetism Program, U.S. Geological Survey

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This page is a summary of: Geoelectric hazard maps for the continental United States, Geophysical Research Letters, September 2016, Wiley,
DOI: 10.1002/2016gl070469.
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