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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Ian R. Mann</dc:contributor>
  <dc:contributor>Timo Qvick</dc:contributor>
  <dc:contributor>Kalevi Mursula</dc:contributor>
  <dc:creator>Jeffrey J. Love</dc:creator>
  <dc:date>2025</dc:date>
  <dc:description>&lt;p&gt;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 −&lt;strong&gt;&lt;i&gt;Dst&lt;/i&gt;&lt;/strong&gt; &amp;gt; &lt;strong&gt;200&lt;/strong&gt; 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 &lt;strong&gt;34&lt;/strong&gt;&lt;span&gt;°&lt;/span&gt;. 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&lt;span&gt;°&lt;/span&gt;. 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 −&lt;strong&gt;&lt;i&gt;Dst&lt;/i&gt;&lt;/strong&gt; = &lt;strong&gt;673&lt;/strong&gt; nT. That this storm occurred just a few days before the Carrington storm of 2 September (maximum −&lt;strong&gt;&lt;i&gt;Dst&lt;/i&gt;&lt;/strong&gt; = &lt;strong&gt;964&lt;/strong&gt; nT) deserves attention. A storm that occurred on 17 September 1770 is estimated to have had maximum −&lt;strong&gt;&lt;i&gt;Dst&lt;/i&gt;&lt;/strong&gt; = &lt;strong&gt;928&lt;/strong&gt; nT. The vision of Ezekiel could have been inspired by aurorae from a storm with maximum −&lt;i&gt;&lt;strong&gt;Dst&lt;/strong&gt;&lt;/i&gt; = &lt;strong&gt;550&lt;/strong&gt; nT.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2024SW004286</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>What is the lowest latitude of discrete aurorae during superstorms?</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>