Articles | Volume 19, issue 14
Atmos. Chem. Phys., 19, 9485–9494, 2019
https://doi.org/10.5194/acp-19-9485-2019
Atmos. Chem. Phys., 19, 9485–9494, 2019
https://doi.org/10.5194/acp-19-9485-2019

Research article 26 Jul 2019

Research article | 26 Jul 2019

Reactive nitrogen (NOy) and ozone responses to energetic electron precipitation during Southern Hemisphere winter

Pavle Arsenovic et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Lorena Grabowski on behalf of the Authors (17 Apr 2019)  Author's response
ED: Referee Nomination & Report Request started (03 May 2019) by Gabriele Stiller
RR by Anonymous Referee #2 (17 May 2019)
RR by Anonymous Referee #3 (19 May 2019)
ED: Publish subject to minor revisions (review by editor) (01 Jun 2019) by Gabriele Stiller
AR by Anna Wenzel on behalf of the Authors (06 Jun 2019)  Author's response    Manuscript
ED: Publish as is (18 Jun 2019) by Gabriele Stiller
Download
Short summary
Low-energy electrons (LEE) are the dominant source of odd nitrogen, which destroys ozone, in the mesosphere and stratosphere in polar winter in the geomagnetically active periods. However, the observed stratospheric ozone anomalies can be reproduced only when accounting for both low- and middle-range energy electrons (MEE) in the chemistry-climate model. Ozone changes may induce further dynamical and thermal changes in the atmosphere. We recommend including both LEE and MEE in climate models.
Altmetrics
Final-revised paper
Preprint