Articles | Volume 24, issue 10
https://doi.org/10.5194/acp-24-5971-2024
https://doi.org/10.5194/acp-24-5971-2024
Research article
 | 
24 May 2024
Research article |  | 24 May 2024

The effects of warm-air intrusions in the high Arctic on cirrus clouds

Georgios Dekoutsidis, Martin Wirth, and Silke Groß

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2708', Anonymous Referee #1, 04 Jan 2024
  • RC2: 'Comment on egusphere-2023-2708', Eleni Marinou, 15 Feb 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Georgios Dekoutsidis on behalf of the Authors (11 Mar 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (23 Mar 2024) by Timothy Garrett
AR by Georgios Dekoutsidis on behalf of the Authors (29 Mar 2024)
Download
Short summary
For decades the earth's temperature has been rising. The Arctic regions are warming faster. Cirrus clouds can contribute to this phenomenon. During warm-air intrusions, air masses are transported into the Arctic from the mid-latitudes. The HALO-(AC)3 campaign took place to measure cirrus during intrusion events and under normal conditions. We study the two cloud types based on these measurements and find differences in their geometry, relative humidity distribution and vertical structure.
Altmetrics
Final-revised paper
Preprint