Articles | Volume 21, issue 19
Atmos. Chem. Phys., 21, 14941–14958, 2021
https://doi.org/10.5194/acp-21-14941-2021
Atmos. Chem. Phys., 21, 14941–14958, 2021
https://doi.org/10.5194/acp-21-14941-2021

Research article 08 Oct 2021

Research article | 08 Oct 2021

Understanding the surface temperature response and its uncertainty to CO2, CH4, black carbon, and sulfate

Kalle Nordling et al.

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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 acp-2021-401', Anonymous Referee #2, 16 Jul 2021
    • AC1: 'Reply on RC1', Kalle Nordling, 06 Sep 2021
  • RC2: 'Comment on acp-2021-401', William Collins, 18 Jul 2021
    • AC2: 'Reply on RC2', Kalle Nordling, 06 Sep 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Kalle Nordling on behalf of the Authors (06 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (15 Sep 2021) by Tanja Schuck
AR by Kalle Nordling on behalf of the Authors (16 Sep 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (16 Sep 2021) by Tanja Schuck
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Short summary
Understanding the temperature responses to different climate forcing agents, such as greenhouse gases and aerosols, is crucial for understanding future regional climate changes. In climate models, the regional temperature responses vary for all forcing agents, but the causes of this variability are poorly understood. For all forcing agents, the main component contributing to variance in regional surface temperature responses between the climate models is the clear-sky longwave emissivity.
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