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Title: The High Latitude Ionospheric Response to the Major May 2024 Geomagnetic Storm: A Synoptic View

Journal Article · · Geophysical Research Letters
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [3];  [4]; ORCiD logo [5];  [6]; ORCiD logo [7]; ORCiD logo [3];  [2]; ORCiD logo [8]; ORCiD logo [4]; ORCiD logo [4]; ORCiD logo [9]; ORCiD logo [2]; ORCiD logo [10]; ORCiD logo [2];  [1]
  1. Space Environment and Radio Engineering Group (SERENE) School of Engineering University of Birmingham Birmingham UK, Department of Physics University of New Brunswick Fredericton NB Canada
  2. Space Environment and Radio Engineering Group (SERENE) School of Engineering University of Birmingham Birmingham UK
  3. Department of Physics University of New Brunswick Fredericton NB Canada
  4. Haystack Observatory Massachusetts Institute of Technology Tyngsborough MA USA
  5. Department of Atmospheric and Oceanic Sciences University of California Los Angeles Los Angeles CA USA
  6. Department of Physics and Applied Physics University of Massachusetts Lowell MA USA
  7. Center for Solar‐Terrestrial Research New Jersey Institute of Technology Newark NJ USA
  8. British Antarctic Survey Cambridge UK
  9. SRI International Menlo Park CA USA
  10. Boston College Chestnut Hill MA USA

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 150–300 km, reaching levels of up to 630 km. 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 eleventh, 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 eleventh.

Sponsoring Organization:
USDOE
OSTI ID:
2473495
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 19 Vol. 51; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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