Articles | Volume 19, issue 9
Atmos. Chem. Phys., 19, 5835–5852, 2019
https://doi.org/10.5194/acp-19-5835-2019
Atmos. Chem. Phys., 19, 5835–5852, 2019
https://doi.org/10.5194/acp-19-5835-2019

Research article 03 May 2019

Research article | 03 May 2019

Dynamic and timing properties of new aerosol particle formation and consecutive growth events

Imre Salma and Zoltán Németh

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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 Svenja Lange on behalf of the Authors (08 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Feb 2019) by Xavier Querol
RR by Anonymous Referee #3 (18 Feb 2019)
RR by Anonymous Referee #5 (13 Mar 2019)
RR by Anonymous Referee #6 (19 Mar 2019)
ED: Reconsider after major revisions (21 Mar 2019) by Xavier Querol
AR by Imre SALMA on behalf of the Authors (01 Apr 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Apr 2019) by Xavier Querol
RR by Anonymous Referee #3 (10 Apr 2019)
RR by Anonymous Referee #6 (21 Apr 2019)
ED: Publish subject to technical corrections (22 Apr 2019) by Xavier Querol
AR by Imre SALMA on behalf of the Authors (23 Apr 2019)  Author's response    Manuscript
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Short summary
Condensing atmospheric chemical species and/or their processes in the city centre seem to contribute equally to new particle formation and particle growth. In the near-city background, however, chemical compounds and their processes power particle growth more than particle formation. There is much indirect evidence that chemical species other than H2SO4 largely influence the particle growth and possibly the atmosphere.
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