Articles | Volume 36, issue 5
https://doi.org/10.5194/angeo-36-1183-2018
https://doi.org/10.5194/angeo-36-1183-2018
Regular paper
 | 
10 Sep 2018
Regular paper |  | 10 Sep 2018

Fast plasma sheet flows and X line motion in the Earth's magnetotail: results from a global hybrid-Vlasov simulation

Liisa Juusola, Sanni Hoilijoki, Yann Pfau-Kempf, Urs Ganse, Riku Jarvinen, Markus Battarbee, Emilia Kilpua, Lucile Turc, and Minna Palmroth

Viewed

Total article views: 2,597 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,995 528 74 2,597 163 105 172
  • HTML: 1,995
  • PDF: 528
  • XML: 74
  • Total: 2,597
  • Supplement: 163
  • BibTeX: 105
  • EndNote: 172
Views and downloads (calculated since 10 Sep 2018)
Cumulative views and downloads (calculated since 10 Sep 2018)
Latest update: 27 Nov 2025
Download
Short summary
The solar wind interacts with the Earth’s magnetic field, forming a magnetosphere. On the night side solar wind stretches the magnetosphere into a long tail. A process called magnetic reconnection opens the magnetic field lines and reconnects them, accelerating particles to high energies. We study this in the magnetotail using a numerical simulation model of the Earth’s magnetosphere. We study the motion of the points where field lines reconnect and the fast flows driven by this process.
Share