EGU25-11029, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-11029
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 15:05–15:15 (CEST)
 
Room L1
Identifying magnetotail jet fronts in a 6D global hybrid-Vlasov simulation
Lauri Pänkäläinen1, Giulia Cozzani2, Markus Battarbee1, Urs Ganse1, Yann Pfau-Kempf1, Jonas Suni1, and Minna Palmroth1,3
Lauri Pänkäläinen et al.
  • 1Department of Physics, University of Helsinki, Helsinki, Finland (lauri.pankalainen@helsinki.fi)
  • 2LPC2E, CNRS, CNES, OSUC, University of Orléans, Orléans, France
  • 3Space and Earth Observation Centre, Finnish Meteorological Institute, Helsinki, Finland

Magnetic reconnection in Earth's magnetotail is thought to create bursty bulk flows (BBFs), short-lived plasma bulk velocity enhancements in the magnetotail's central plasma sheet (CPS) region. Closely related to BBFs are dipolarization fronts (DFs), sudden increases in Bz, the magnetic field component aligned with Earth's magnetic dipole axis. Both phenomena affect energy distribution and flux transport in the magnetotail.

We demonstrate novel methods of identifying BBFs and DFs in a 3D global magnetospheric simulation and present results for multiple case studies. BBFs and DFs are searched for in a simulation conducted using Vlasiator, a global magnetospheric hybrid-Vlasov code where ions are modeled using distribution functions and electrons are treated as a charge-neutralizing fluid. DFs are identified using a magnetic field time derivative threshold dBz /dt > 0.35 nT/s. BBFs are defined based on a velocity threshold, and they are studied on a case-by-case basis. Tailward DFs (anti-dipolarization fronts) are found at magnetic islands, while earthward DFs are mostly seen in finger-like structures of high earthward bulk velocity alongside BBFs. Signatures registered as BBFs in spacecraft view also originate due to moving reconnection locations and movement of the current sheet within the CPS while the reconnection outflow stays roughly constant. The results show that rapid Bz variations in the simulation have multiple sources, and similar satellite measurements of BBFs can arise from different physical phenomena. The findings may help with interpreting satellite observations in the magnetotail.

How to cite: Pänkäläinen, L., Cozzani, G., Battarbee, M., Ganse, U., Pfau-Kempf, Y., Suni, J., and Palmroth, M.: Identifying magnetotail jet fronts in a 6D global hybrid-Vlasov simulation, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-11029, https://doi.org/10.5194/egusphere-egu25-11029, 2025.