Articles | Volume 23, issue 1
Research article
 | Highlight paper
05 Jan 2023
Research article | Highlight paper |  | 05 Jan 2023

Dependence of strategic solar climate intervention on background scenario and model physics

John T. Fasullo and Jadwiga H. Richter


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-779', Alan Robock, 07 Sep 2022
    • AC1: 'Reply on RC1', John Fasullo, 09 Nov 2022
  • RC2: 'Comment on egusphere-2022-779', Douglas MacMartin, 14 Sep 2022
    • AC2: 'Reply on RC2', John Fasullo, 09 Nov 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by John Fasullo on behalf of the Authors (09 Nov 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (22 Nov 2022) by Susannah Burrows
AR by John Fasullo on behalf of the Authors (08 Dec 2022)
Executive editor
Stratospheric aerosol injection (SAI) is often discussed in the media and in policy circles as a possible action to limit future increase in global temperatures. Indeed it has been demonstrated in model simulations that in principle injection could be 'controlled', using model information, to meet specific targets on the temperature increase and its spatial distribution. This paper shows that the simulated climate response to SAI is strongly model-dependent, reflecting fundamental uncertainties in model representation of key processes. In particular this means that the SAI determined by the control algorithms as those required to achieve temperature targets different significantly from one model to another. Specific mechanisms, in particular the difference in rapid response in clouds and in precipitation to an imposed radiative perturbation and the ensuing ocean circulation response, are identified that contribute to the strong differences in model response to SAI. There is also a strong sensitivity to the pre-existing sulphate distribution which will be determined by future anthropogenic emissions. The authors note that these inter-model differences are unlikely to be resolved quickly and that controlled SAI, to achieve specific temperature goals and with well-quantified risks of unexpected consequences, is likely to remain out of reach for many years.
Short summary
The continued high levels of anthropogenic greenhouse gas emissions increase the likelihood that key climate warming thresholds will be exceeded in the coming decades. Here we examine a recently proposed geoengineering approach using two recently produced climate model experiments. We find the associated latitudinal distribution of aerosol mass to exhibit substantial uncertainty, suggesting the need for significant flexibility in the location and amount of aerosol delivery, if implemented.
Final-revised paper