Articles | Volume 40, issue 2
Ann. Geophys., 40, 167–177, 2022
https://doi.org/10.5194/angeo-40-167-2022
Ann. Geophys., 40, 167–177, 2022
https://doi.org/10.5194/angeo-40-167-2022

Regular paper 15 Mar 2022

Regular paper | 15 Mar 2022

Statistical study and corresponding evolution of plasmaspheric plumes under different levels of geomagnetic storms

Haimeng Li et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on angeo-2021-55', Anonymous Referee #1, 12 Dec 2021
    • AC1: 'Reply on RC1', Rongxin Tang, 09 Jan 2022
  • RC2: 'Comment on angeo-2021-55', Anonymous Referee #2, 13 Dec 2021
    • AC2: 'Reply on RC2', Rongxin Tang, 09 Jan 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish as is (25 Jan 2022) by Jonathan Rae
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Short summary
The plasmaspheric plume is an important region of detached plasma elements and provides an effective coupling channel of energy/mass between the inner magnetospheric plasmasphere and outer magnetosphere. In this study, using Van Allen Probe data, we present a statistical result of plasmaspheric plumes in the inner magnetosphere, which implies that the plumes tend to occur during the recovery phase of geomagnetic storms, and the occurrence rate is larger during stronger geomagnetic activity.