The high latitude ionospheric response to the major May 2024 geomagnetic
storm: A synoptic view
- 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
Anthea Coster
Massachusetts Institute of Technology Haystack
Author ProfileLindsay Victoria Goodwin
New Jersey Institute of Technology
Author ProfileLarisa Goncharenko
MIT Haystack Observatory, Westford, MA, USA.
Author ProfileAbstract
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