Articles | Volume 11, issue 8
https://doi.org/10.5194/gmd-11-3261-2018
https://doi.org/10.5194/gmd-11-3261-2018
Model description paper
 | 
13 Aug 2018
Model description paper |  | 13 Aug 2018

A parameterisation for the co-condensation of semi-volatile organics into multiple aerosol particle modes

Matthew Crooks, Paul Connolly, and Gordon McFiggans

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Matthew Crooks on behalf of the Authors (15 Feb 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (02 Mar 2018) by Klaus Gierens
AR by Matthew Crooks on behalf of the Authors (05 Apr 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (17 Apr 2018) by Klaus Gierens
ED: Publish as is (19 Apr 2018) by Klaus Gierens
AR by Matthew Crooks on behalf of the Authors (29 Apr 2018)  Manuscript 
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Short summary
Clouds form when water condenses onto particles in the atmosphere and the size and chemical composition of these particles can have a large influence over how much water condenses and the subsequent formation of cloud. Additional gases exist in the atmosphere that can condense onto the aerosol particles and change their composition. We present a fast and efficient method of calculating the effect of atmospheric gases on the formation of cloud that can be used in climate and weather models.