Articles | Volume 25, issue 6
https://doi.org/10.5194/acp-25-3717-2025
https://doi.org/10.5194/acp-25-3717-2025
Research article
 | 
27 Mar 2025
Research article |  | 27 Mar 2025

Spatiotemporal variations of stratospheric aerosol size between 2002 and 2005 from measurements with SAGE III/M3M

Felix Wrana, Terry Deshler, Christian Löns, Larry W. Thomason, and Christian von Savigny

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2942', Anonymous Referee #1, 24 Oct 2024
    • RC2: 'Reply on RC1', Anonymous Referee #1, 24 Oct 2024
    • AC1: 'Reply on RC1', Felix Wrana, 17 Dec 2024
  • RC3: 'Comment on egusphere-2024-2942', Filip Vanhellemont, 07 Nov 2024
    • AC2: 'Reply on RC3', Felix Wrana, 17 Dec 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Felix Wrana on behalf of the Authors (20 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (23 Dec 2024) by John Plane
AR by Felix Wrana on behalf of the Authors (02 Jan 2025)
Download
Short summary
There is a natural and globally occurring layer of small droplets (aerosols) at roughly 20 km altitude in the atmosphere. In this work, the size of these droplets is calculated from satellite measurements for the years 2002 to 2005, which is important for the aerosol cooling effect on Earth's climate. These years are interesting because there were no large volcanic eruptions that would change the background state of the aerosols. The results are compared to reliable balloon-borne measurements.
Share
Altmetrics
Final-revised paper
Preprint