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The high latitude ionospheric response to the major May 2024 geomagnetic storm: A synoptic view
  • +15
  • David R. Themens,
  • Sean Elvidge,
  • Anthony Mark McCaffrey,
  • P. T. Jayachandran,
  • Anthea Coster,
  • Roger H Varney,
  • Ivan Galkin,
  • Lindsay Victoria Goodwin,
  • Chris Watson,
  • Sophie Maguire,
  • Andrew John Kavanagh,
  • Shun-Rong Zhang,
  • Larisa Goncharenko,
  • Asti Bhatt,
  • Gareth Dorrian,
  • Keith M. Groves,
  • Alan George Wood,
  • Benjamin Reid
David R. Themens
University of Birmingham

Corresponding Author:[email protected]

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Sean Elvidge
University of Birmingham
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Anthony Mark McCaffrey
University of New Brunswick
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P. T. Jayachandran
University of New Brunswick
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Anthea Coster
Massachusetts Institute of Technology Haystack
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Roger H Varney
University of California, Los Angeles
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Ivan Galkin
UMass Lowell, Space Science Lab
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Lindsay Victoria Goodwin
New Jersey Institute of Technology
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Chris Watson
University of New Brunswick
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Sophie Maguire
University of Birmingham
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Andrew John Kavanagh
British Antarctic Survey
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Shun-Rong Zhang
MIT Haystack Observatory
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Larisa Goncharenko
MIT Haystack Observatory, Westford, MA, USA.
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Asti Bhatt
SRI International
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Gareth Dorrian
University of Birmingham
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Keith M. Groves
Air Force Research Laboratory
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Alan George Wood
University of Birmingham
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Benjamin Reid
University of Birmingham
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Abstract

The high latitude ionospheric evolution of the May 10-11, 2024, geomagnetic storm is investigated in terms of Total Electron Content and contextualized with Incoherent Scatter Radar and ionosonde observations. Substantial plasma lifting is observed within the initial Storm Enhanced Density plume with ionospheric peak heights increasing by 150km to 300km, reaching levels of up to 630km. Scintillation is observed within the cusp during the initial expansion phase of the storm, spreading across the auroral oval thereafter. Patch transport into the polar cap produces broad regions of scintillation that are rapidly cleared from the region after a strong Interplanetary Magnetic Field reversal at 2230UT. Strong heating and composition changes result in the complete absence of the F2-layer on the 11th, suffocating high latitude convection from dense plasma necessary for Tongue of Ionization and patch formation, ultimately resulting in a suppression of polar cap scintillation on the 11th.
31 Jul 2024Submitted to ESS Open Archive
01 Aug 2024Published in ESS Open Archive