Articles | Volume 18, issue 2
Atmos. Chem. Phys., 18, 1291–1306, 2018
https://doi.org/10.5194/acp-18-1291-2018
Atmos. Chem. Phys., 18, 1291–1306, 2018
https://doi.org/10.5194/acp-18-1291-2018

Research article 31 Jan 2018

Research article | 31 Jan 2018

Long-term (2001–2012) trends of carbonaceous aerosols from a remote island in the western North Pacific: an outflow region of Asian pollutants

Suresh K. R. Boreddy et al.

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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 Suresh Kumar Reddy Boreddy on behalf of the Authors (06 Jul 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (12 Jul 2017) by Stefania Gilardoni
RR by Anonymous Referee #1 (21 Jul 2017)
RR by Anonymous Referee #2 (24 Jul 2017)
ED: Reconsider after major revisions (02 Aug 2017) by Stefania Gilardoni
AR by Suresh Kumar Reddy Boreddy on behalf of the Authors (13 Sep 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Oct 2017) by Stefania Gilardoni
RR by Anonymous Referee #1 (16 Oct 2017)
RR by Anonymous Referee #2 (17 Oct 2017)
ED: Publish subject to minor revisions (review by editor) (26 Oct 2017) by Stefania Gilardoni
AR by Suresh Kumar Reddy Boreddy on behalf of the Authors (05 Nov 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (15 Nov 2017) by Stefania Gilardoni
AR by Suresh Kumar Reddy Boreddy on behalf of the Authors (25 Nov 2017)  Author's response    Manuscript
ED: Publish as is (20 Dec 2017) by Stefania Gilardoni
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Short summary
To better understand the impact of long-range atmospheric transport of East Asian pollutants over the western North Pacific, we conducted a long-term (2001–12) study on carbonaceous aerosols over the WNP, which demonstrates that the photochemical formation of WSOC and its contributions to SOA have increased over the western North Pacific via long-range atmospheric transport. Biomass-burning-derived carbonaceous aerosols have increased, while primary fossil-fuel-derived aerosols have decreased.
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