Characterization and source apportionment of organic aerosol at 260&thinsp;m on a meteorological tower in Beijing, China

Zhou, Wei; Wang, Qingqing; Zhao, Xiujuan; Xu, Weiqi; Chen, Chen; Du, Wei; Zhao, Jian; Canonaco, Francesco; Prévôt, André S. H.; Fu, Pingqing; Wang, Zifa; Worsnop, Douglas R.; Sun, Yele

doi:https://doi.org/10.5194/acp-18-3951-2018

Articles | Volume 18, issue 6

https://doi.org/10.5194/acp-18-3951-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-18-3951-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 6

Research article

|

20 Mar 2018

Research article |

| 20 Mar 2018

Characterization and source apportionment of organic aerosol at 260 m on a meteorological tower in Beijing, China

Wei Zhou, Qingqing Wang, Xiujuan Zhao, Weiqi Xu, Chen Chen, Wei Du, Jian Zhao, Francesco Canonaco, André S. H. Prévôt, Pingqing Fu, Zifa Wang, Douglas R. Worsnop, and Yele Sun

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Final revised paper (published on 20 Mar 2018)
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Preprint (discussion started on 21 Dec 2017)
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Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Comments to acp-2017-1039', Anonymous Referee #3, 11 Jan 2018
RC2: 'Reviewer comment', Anonymous Referee #1, 19 Jan 2018
RC3: '260m vs ground PM1 in beijing', Anonymous Referee #2, 20 Jan 2018
AC1: 'Reply to three reviewers' comments', Yele Sun, 20 Feb 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Yele Sun on behalf of the Authors (20 Feb 2018) Author's response Manuscript

ED: Publish as is (25 Feb 2018) by Fangqun Yu

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Short summary

We present a 3-month analysis of submicron aerosols that were measured at 260 m on a meteorological tower in Beijing, China. The sources of organic aerosol (OA) were analyzed by using a multi-linear engine (ME-2). Our results showed significant changes in both primary and secondary OA composition from the non-heating season to the heating season. We also observed a considerable contribution (10–13%) of cooking OA at 260 m and very different OA composition between ground level and 260 m.