nerc.ac.uk

The 2024 May event in the context of auroral activity over the past 375 yr

Lockwood, Mike ORCID: https://orcid.org/0000-0002-7397-2172; Owens, Mathew J. ORCID: https://orcid.org/0000-0003-2061-2453; Brown, William ORCID: https://orcid.org/0000-0001-9045-9787; Vázquez, Manuel. 2025 The 2024 May event in the context of auroral activity over the past 375 yr. Monthly Notices of the Royal Astronomical Society, 540 (4). 3596-3624. 10.1093/mnras/staf827

Before downloading, please read NORA policies.
[thumbnail of Open Access Paper]
Preview
Text (Open Access Paper)
Lockwood et al 2025 - The 2024 May event in the context of auroral activity over the past 375 yr.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (3MB) | Preview

Abstract/Summary

We survey 223 916 auroral records from the Northern hemisphere observed between 1650 January and 2024 July, making full allowance for the secular change in the geomagnetic field. We generate criteria for defining extreme auroral events that are met on 0.015 per cent and 0.023 per cent of nights since 1650 and 1790, respectively. After discussing biases and trends in the data, we compare the event of 2024 May 10–11 with other extreme events and investigate the connections to geomagnetic and sunspot activity. Ranking the events by the lowest geomagnetic latitude from which aurora was observed, the second night of the 2024 May event is shown to be the third most extensive known, the most extensive being 1872 February 4. Allowing for dark adaptation of human vision, we find no evidence that this ranking has been greatly influenced by the increased use of modern digital cameras. We show that the area of the sunspot group from where the causal coronal mass ejection arises (identified by the associated flare) is weakly anticorrelated with the auroral and geomagnetic response; the scatter being large such that, although the 1872 February event arose from a rather small sunspot group, the 2024 May event arose from a large group, as did the ‘Carrington Events’ of 1859 August/September (ranked 2, 4, and 5). We show that the extreme events all occur during Carrington rotations for which the average open solar flux, F_{s} exceeds 4x10^{14}Wb but only 3.6 per cent of Carrington rotations when F_{s} exceeds this value give an extreme event at Earth.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1093/mnras/staf827
Additional Keywords: geomagnetism, space weather
NORA Subject Terms: Earth Sciences
Date made live: 04 Jul 2025 10:43 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/539774

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...