Articles | Volume 16, issue 3
https://doi.org/10.5194/esd-16-667-2025
https://doi.org/10.5194/esd-16-667-2025
Research article
 | 
05 May 2025
Research article |  | 05 May 2025

Change in negative emission burden between an overshoot versus peak-shaved stratospheric aerosol injection pathway

Susanne Baur, Benjamin M. Sanderson, Roland Séférian, and Laurent Terray

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Reviewer comment on egusphere-2024-2344', Anonymous Referee #1, 10 Oct 2024
  • RC2: 'Comment on egusphere-2024-2344', Anonymous Referee #2, 17 Oct 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (20 Dec 2024) by Gabriele Messori
AR by Susanne Baur on behalf of the Authors (28 Jan 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 Jan 2025) by Gabriele Messori
RR by Anonymous Referee #2 (08 Feb 2025)
RR by Anonymous Referee #1 (15 Feb 2025)
ED: Publish as is (16 Feb 2025) by Gabriele Messori
AR by Susanne Baur on behalf of the Authors (24 Feb 2025)
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Short summary
Stratospheric aerosol injection (SAI) could be used alongside mitigation to reduce global warming. Previous studies suggest that more atmospheric CO2 is taken up when SAI is deployed. Here, we look at the entire SAI deployment from start to after termination. We show how the initial CO2 uptake benefit, and hence lower mitigation burden, is reduced in later stages of SAI, where the reduction in natural CO2 uptake turns into an additional mitigation burden. 
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