Articles | Volume 20, issue 1
https://doi.org/10.5194/acp-20-457-2020
https://doi.org/10.5194/acp-20-457-2020
Research article
 | 
14 Jan 2020
Research article |  | 14 Jan 2020

Satellite observations of aerosols and clouds over southern China from 2006 to 2015: analysis of changes and possible interaction mechanisms

Nikos Benas, Jan Fokke Meirink, Karl-Göran Karlsson, Martin Stengel, and Piet Stammes

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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 Nikos Benas on behalf of the Authors (15 Feb 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (25 Feb 2019) by Toshihiko Takemura
RR by Stefan Kinne (21 Mar 2019)
RR by Anonymous Referee #3 (07 May 2019)
ED: Reconsider after major revisions (07 May 2019) by Toshihiko Takemura
AR by Nikos Benas on behalf of the Authors (18 Jun 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 Jun 2019) by Toshihiko Takemura
RR by Anonymous Referee #3 (07 Jul 2019)
ED: Reconsider after major revisions (07 Jul 2019) by Toshihiko Takemura
AR by Nikos Benas on behalf of the Authors (16 Aug 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 Aug 2019) by Toshihiko Takemura
RR by Anonymous Referee #3 (16 Sep 2019)
ED: Reconsider after major revisions (16 Sep 2019) by Toshihiko Takemura
AR by Nikos Benas on behalf of the Authors (09 Oct 2019)
ED: Publish as is (29 Nov 2019) by Toshihiko Takemura
AR by Nikos Benas on behalf of the Authors (02 Dec 2019)
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Short summary
In this study we analyse aerosol and cloud changes over southern China from 2006 to 2015 and investigate their possible interaction mechanisms. Results show decreasing aerosol loads and increasing liquid cloud cover in late autumn. Further analysis based on various satellite data sets shows consistency with the aerosol semi-direct effect, whereby less absorbing aerosols in the cloud layer would lead to an overall decrease in the evaporation of cloud droplets, thus increasing cloud amount.
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