Articles | Volume 18, issue 16
https://doi.org/10.5194/acp-18-11581-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-11581-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Production of N2O5 and ClNO2 in summer in urban Beijing, China
Wei Zhou
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Jian Zhao
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Bin Ouyang
Department of Chemistry, University of Cambridge, Cambridge CB2 1EW,
UK
Archit Mehra
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
Weiqi Xu
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Yuying Wang
College of Global Change and Earth System Science, Beijing Normal
University, Beijing 100875, China
Thomas J. Bannan
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
Stephen D. Worrall
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
now at: School of Materials, University of Manchester M13 9PL, UK
Michael Priestley
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
Asan Bacak
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
College of Environmental Sciences and Engineering, Peking University,
Beijing 100871, China
Conghui Xie
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Qingqing Wang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Junfeng Wang
School of Environmental Science and Engineering, Nanjing University of
Information Science and Technology, Nanjing 210044, China
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Yingjie Zhang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Xinlei Ge
School of Environmental Science and Engineering, Nanjing University of
Information Science and Technology, Nanjing 210044, China
Penglin Ye
Aerodyne Research, Inc., Billerica, Massachusetts 01821, USA
Nanjing DiLu Scientific Instrument Inc, Nanjing 210036, China
James D. Lee
National Centre for Atmospheric Science, University of York,
Heslington, York YO10 5DD, UK
Pingqing Fu
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Zifa Wang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Douglas Worsnop
Aerodyne Research, Inc., Billerica, Massachusetts 01821, USA
Roderic Jones
Department of Chemistry, University of Cambridge, Cambridge CB2 1EW,
UK
Carl J. Percival
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
now at: Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA
Centre for Atmospheric Science, School of Earth, Atmospheric and
Environmental Science, University of Manchester, Manchester M13 9PL, UK
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
University of Chinese Academy of Sciences, Beijing 100049, China
Center for Excellence in Regional Atmospheric Environment, Institute
of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
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- Final revised paper (published on 16 Aug 2018)
- Supplement to the final revised paper
- Preprint (discussion started on 04 Apr 2018)
- Supplement to the preprint
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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- Supplement
- RC1: 'Review of acp-2018-348', Anonymous Referee #1, 27 Apr 2018
- RC2: 'Review of “Production of N2O5 and ClNO2 in summer in urban Beijing, China” by Zhou et al.', Anonymous Referee #2, 08 Jun 2018
- AC1: 'Reply to the two referees' comments', Yele Sun, 18 Jul 2018
Peer-review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Yele Sun on behalf of the Authors (18 Jul 2018)
Author's response
Manuscript
ED: Publish subject to technical corrections (26 Jul 2018) by Yongjie Li
AR by Yele Sun on behalf of the Authors (27 Jul 2018)
Manuscript
Short summary
We present measurements of gas-phase N2O5 and ClNO2 by ToF-CIMS during summer in urban Beijing as part of the APHH campaign. High reactivity of N2O5 indicative of active nocturnal chemistry was observed. The lifetime of N2O5 as a function of aerosol surface area and relative humidity was characterized, and N2O5 uptake coefficients were estimated. We also found that the N2O5 loss in this study is mainly attributed to its indirect loss via reactions of NO3 with VOCs and NO.
We present measurements of gas-phase N2O5 and ClNO2 by ToF-CIMS during summer in urban Beijing...
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Preprint