Articles | Volume 16, issue 1
https://doi.org/10.5194/acp-16-305-2016
https://doi.org/10.5194/acp-16-305-2016
Research article
 | 
18 Jan 2016
Research article |  | 18 Jan 2016

Radiative and climate impacts of a large volcanic eruption during stratospheric sulfur geoengineering

A. Laakso, H. Kokkola, A.-I. Partanen, U. Niemeier, C. Timmreck, K. E. J. Lehtinen, H. Hakkarainen, and H. Korhonen

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 Anton Laakso on behalf of the Authors (19 Nov 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (25 Nov 2015) by Jens-Uwe Grooß
RR by Anonymous Referee #2 (15 Dec 2015)
ED: Reconsider after minor revisions (Editor review) (15 Dec 2015) by Jens-Uwe Grooß
AR by Anton Laakso on behalf of the Authors (21 Dec 2015)  Author's response   Manuscript 
ED: Publish as is (22 Dec 2015) by Jens-Uwe Grooß
AR by Anton Laakso on behalf of the Authors (22 Dec 2015)
Download
Short summary
We have studied the impacts of a volcanic eruption during solar radiation management (SRM) using an aerosol-climate model ECHAM5-HAM-SALSA and an Earth system model MPI-ESM. A volcanic eruption during stratospheric sulfur geoengineering would lead to larger particles and smaller amount of new particles than if an volcano erupts in normal atmospheric conditions. Thus, volcanic eruption during SRM would lead to only a small additional cooling which would last for a significantly shorter period.
Altmetrics
Final-revised paper
Preprint