Articles | Volume 21, issue 2
https://doi.org/10.5194/acp-21-1105-2021
https://doi.org/10.5194/acp-21-1105-2021
Research article
 | 
27 Jan 2021
Research article |  | 27 Jan 2021

Climate-driven chemistry and aerosol feedbacks in CMIP6 Earth system models

Gillian Thornhill, William Collins, Dirk Olivié, Ragnhild B. Skeie, Alex Archibald, Susanne Bauer, Ramiro Checa-Garcia, Stephanie Fiedler, Gerd Folberth, Ada Gjermundsen, Larry Horowitz, Jean-Francois Lamarque, Martine Michou, Jane Mulcahy, Pierre Nabat, Vaishali Naik, Fiona M. O'Connor, Fabien Paulot, Michael Schulz, Catherine E. Scott, Roland Séférian, Chris Smith, Toshihiko Takemura, Simone Tilmes, Kostas Tsigaridis, and James Weber

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by William Collins on behalf of the Authors (22 Oct 2020)  Author's response   Manuscript 
ED: Publish as is (06 Nov 2020) by Holger Tost
AR by William Collins on behalf of the Authors (16 Nov 2020)  Author's response   Manuscript 
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Short summary
We find that increased temperatures affect aerosols and reactive gases by changing natural emissions and their rates of removal from the atmosphere. Changing the composition of these species in the atmosphere affects the radiative budget of the climate system and therefore amplifies or dampens the climate response of climate models of the Earth system. This study found that the largest effect is a dampening of climate change as warmer temperatures increase the emissions of cooling aerosols.
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