Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Xiyuan Chi
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Shidong Fan
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Haicong Zhan
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Hui Kang
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Key Lab of Environmental Optics and Technology, Anhui Institute of
Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, Anhui 230031, China
Center for Excellence in Urban Atmospheric Environment, Institute of
Urban Environment, Chinese Academy of Sciences, Xiamen, Fujian 361021, China
Anhui Province Key Laboratory of Polar Environment and Global Change,
School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China
Key Lab of Environmental Optics and Technology, Anhui Institute of
Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei, Anhui 230031, China
Center for Excellence in Urban Atmospheric Environment, Institute of
Urban Environment, Chinese Academy of Sciences, Xiamen, Fujian 361021, China
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Total article views: 6,754 (including HTML, PDF, and XML)
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EndNote
4,445
2,177
132
6,754
803
100
220
HTML: 4,445
PDF: 2,177
XML: 132
Total: 6,754
Supplement: 803
BibTeX: 100
EndNote: 220
Views and downloads (calculated since 06 Nov 2017)
Cumulative views and downloads
(calculated since 06 Nov 2017)
Total article views: 5,677 (including HTML, PDF, and XML)
HTML
PDF
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Total
Supplement
BibTeX
EndNote
3,764
1,791
122
5,677
292
87
201
HTML: 3,764
PDF: 1,791
XML: 122
Total: 5,677
Supplement: 292
BibTeX: 87
EndNote: 201
Views and downloads (calculated since 23 Apr 2018)
Cumulative views and downloads
(calculated since 23 Apr 2018)
Total article views: 1,077 (including HTML, PDF, and XML)
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Total
Supplement
BibTeX
EndNote
681
386
10
1,077
511
13
19
HTML: 681
PDF: 386
XML: 10
Total: 1,077
Supplement: 511
BibTeX: 13
EndNote: 19
Views and downloads (calculated since 06 Nov 2017)
Cumulative views and downloads
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Total article views: 6,754 (including HTML, PDF, and XML)
Thereof 6,576 with geography defined
and 178 with unknown origin.
Total article views: 5,677 (including HTML, PDF, and XML)
Thereof 5,526 with geography defined
and 151 with unknown origin.
Total article views: 1,077 (including HTML, PDF, and XML)
Thereof 1,050 with geography defined
and 27 with unknown origin.
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We use observations of the oxygen isotopic composition of sulfate aerosol as a fingerprint to quantify various sulfate formation mechanisms during pollution events in Beijing, China. We found that heterogeneous reactions on aerosols dominated sulfate production in general; however, in-cloud reactions would dominate haze sulfate production when cloud liquid water content was high. The findings also suggest the heterogeneity of aerosol acidity should be parameterized in models.
We use observations of the oxygen isotopic composition of sulfate aerosol as a fingerprint to...
