Articles | Volume 38, issue 2
https://doi.org/10.5194/angeo-38-491-2020
https://doi.org/10.5194/angeo-38-491-2020
Regular paper
 | 
08 Apr 2020
Regular paper |  | 08 Apr 2020

Estimating the fate of oxygen ion outflow from the high-altitude cusp

Patrik Krcelic, Stein Haaland, Lukas Maes, Rikard Slapak, and Audrey Schillings

Viewed

Total article views: 3,660 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,755 791 114 3,660 179 223
  • HTML: 2,755
  • PDF: 791
  • XML: 114
  • Total: 3,660
  • BibTeX: 179
  • EndNote: 223
Views and downloads (calculated since 30 Aug 2019)
Cumulative views and downloads (calculated since 30 Aug 2019)

Viewed (geographical distribution)

Total article views: 3,660 (including HTML, PDF, and XML) Thereof 3,295 with geography defined and 365 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 18 May 2026
Download
Short summary
In this paper we have used Cluster EDI data in combination with the CODIF cusp dataset from Slapak et al. (2017) to obtain parallel and convection velocities for oxygen ions; 69 % of total oxygen outflow from the high-altitude cusps escapes the magnetosphere on average; 50 % escapes tailward beyond the distant X-line. The oxygen capture-versus-escape ratio is highly dependent on geomagnetic conditions. During active conditions, the majority of oxygen outflow is convected to the plasma sheet.
Share