State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
College of Earth Sciences, University of Chinese Academy of Sciences,
Beijing 100049, China
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
College of Earth Sciences, University of Chinese Academy of Sciences,
Beijing 100049, China
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Nanjing University of Information Science &
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
Qingqing Wang
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Chen Chen
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Weiqi Xu
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
College of Earth Sciences, University of Chinese Academy of Sciences,
Beijing 100049, China
Tingting Han
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
College of Earth Sciences, 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
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, 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
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing 100029, China
Center for Excellence in Urban Atmospheric Environment, Institute of
Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
College of Earth Sciences, University of Chinese Academy of Sciences,
Beijing 100049, China
Viewed
Total article views: 5,065 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,468
1,488
109
5,065
762
127
201
HTML: 3,468
PDF: 1,488
XML: 109
Total: 5,065
Supplement: 762
BibTeX: 127
EndNote: 201
Views and downloads (calculated since 08 Sep 2016)
Cumulative views and downloads
(calculated since 08 Sep 2016)
Total article views: 4,448 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,094
1,264
90
4,448
498
115
176
HTML: 3,094
PDF: 1,264
XML: 90
Total: 4,448
Supplement: 498
BibTeX: 115
EndNote: 176
Views and downloads (calculated since 03 Mar 2017)
Cumulative views and downloads
(calculated since 03 Mar 2017)
Total article views: 617 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
374
224
19
617
264
12
25
HTML: 374
PDF: 224
XML: 19
Total: 617
Supplement: 264
BibTeX: 12
EndNote: 25
Views and downloads (calculated since 08 Sep 2016)
Cumulative views and downloads
(calculated since 08 Sep 2016)
Viewed (geographical distribution)
Total article views: 5,065 (including HTML, PDF, and XML)
Thereof 5,059 with geography defined
and 6 with unknown origin.
Total article views: 4,448 (including HTML, PDF, and XML)
Thereof 4,447 with geography defined
and 1 with unknown origin.
Total article views: 617 (including HTML, PDF, and XML)
Thereof 612 with geography defined
and 5 with unknown origin.
We conducted aerosol particle composition measurements at ground level and 260 m with two aerosol mass spectrometers in Beijing during the 2015 China Victory Day parade. Our results showed a stronger impact of emission controls on inorganic aerosol than OA. A larger decrease in more oxidized SOA than the less oxidized one during the control period was also observed. Our results indicate that emission controls and the changes in meteorological conditions have affected SOA formation mechanisms.
We conducted aerosol particle composition measurements at ground level and 260 m with two...