Articles | Volume 13, issue 4
https://doi.org/10.5194/esd-13-1535-2022
https://doi.org/10.5194/esd-13-1535-2022
Research article
 | 
07 Nov 2022
Research article |  | 07 Nov 2022

On the additivity of climate responses to the volcanic and solar forcing in the early 19th century

Shih-Wei Fang, Claudia Timmreck, Johann Jungclaus, Kirstin Krüger, and Hauke Schmidt

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-638', Anonymous Referee #1, 13 Sep 2022
    • AC1: 'Reply on RC1', Shih-Wei Fang, 16 Oct 2022
  • RC2: 'Comment on egusphere-2022-638', Ewa Bednarz, 19 Sep 2022
    • AC1: 'Reply on RC1', Shih-Wei Fang, 16 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (17 Oct 2022) by Ben Kravitz
AR by Shih-Wei Fang on behalf of the Authors (17 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (18 Oct 2022) by Ben Kravitz
AR by Shih-Wei Fang on behalf of the Authors (21 Oct 2022)  Author's response   Manuscript 
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Short summary
The early 19th century was the coldest period over the past 500 years, when strong tropical volcanic events and a solar minimum coincided. This study quantifies potential surface cooling from the solar and volcanic forcing in the early 19th century with large ensemble simulations, and identifies the regions that their impacts cannot be simply additive. The cooling perspective of Arctic amplification exists in both solar and post-volcano period with the albedo feedback as the main contribution.
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