Articles | Volume 18, issue 4
Atmos. Chem. Phys., 18, 2363–2380, 2018
https://doi.org/10.5194/acp-18-2363-2018

Special issue: The CERN CLOUD experiment (ACP/AMT inter-journal SI)

Atmos. Chem. Phys., 18, 2363–2380, 2018
https://doi.org/10.5194/acp-18-2363-2018

Research article 19 Feb 2018

Research article | 19 Feb 2018

Measurement–model comparison of stabilized Criegee intermediate and highly oxygenated molecule production in the CLOUD chamber

Nina Sarnela et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nina Sarnela on behalf of the Authors (21 Dec 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (02 Jan 2018) by Frank Keutsch
AR by Nina Sarnela on behalf of the Authors (08 Jan 2018)  Author's response    Manuscript
ED: Publish as is (09 Jan 2018) by Frank Keutsch
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Short summary
Atmospheric trace gases can form small molecular clusters, which can grow to larger sizes through the condensation of vapours. This process is called new particle formation. In this paper we studied the formation of sulfuric acid and highly oxygenated molecules, the key compounds in atmospheric new particle formation, in chamber experiments and introduced a way to simulate these ozonolysis products of α-pinene in a simple manner.
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