What Is the Lowest Latitude of Discrete Aurorae During Superstorms?

Abstract From a survey of published accounts of visual sightings of aurorae, a compilation is presented of the lowest identified geomagnetic latitude at which discrete aurorae were seen at local zenith during magnetic storms having intensities with maximum −Dst>200 nT. The compilation includes da...

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Bibliographic Details
Main Authors: Jeffrey J. Love, Ian R. Mann, Timo Qvick, Kalevi Mursula
Format: Article
Language:English
Published: Wiley 2025-04-01
Series:Space Weather
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Online Access:https://doi.org/10.1029/2024SW004286
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Summary:Abstract From a survey of published accounts of visual sightings of aurorae, a compilation is presented of the lowest identified geomagnetic latitude at which discrete aurorae were seen at local zenith during magnetic storms having intensities with maximum −Dst>200 nT. The compilation includes data for the superstorms of 2 September 1859, 4 February 1872, and 15 May 1921. A statistical model is developed representing the equatorward boundary of discrete aurorae versus storm intensity. The model indicates that a once‐per‐century storm would likely induce discrete aurorae at zenith down to a geomagnetic latitude of 34°. Insofar as aurorae can be taken as a proxy for electrojet currents, such a storm would expose many nighttime electric‐power systems in the contiguous United States or Europe to high levels of geomagnetic disturbance. A Carrington‐class storm would induce discrete aurorae down to 24°. These exposures are much greater than those indicated in recent numerical simulations of extreme magnetic storms. Using the model to infer storm intensity from reports of low‐latitude aurorae, a storm on 28 August 1859 likely had maximum −Dst=673 nT. That this storm occurred just a few days before the Carrington storm of 2 September (maximum −Dst=964 nT) deserves attention. A storm that occurred on 17 September 1770 is estimated to have had maximum −Dst=928 nT. A vision described by Ezekiel could have been inspired by aurorae from a storm with maximum −Dst=550 nT.
ISSN:1542-7390