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
Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang
University, Hangzhou, Zhejiang, 310027, China
Xiaoyong Liu
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 Regional Atmospheric Environment, Chinese
Academy of Science, Xiamen, 361021, China
Xueshun Chen
State Key Laboratory of Atmospheric Boundary Layer Physics and
Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of
Sciences, Beijing, 100029, China
Yu Tian
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
College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China
Center for Excellence in Regional Atmospheric Environment, Chinese
Academy of Science, Xiamen, 361021, China
Institute of Surface-Earth System Science, Tianjin University, Tianjin,
300072, 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
College of Earth Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China
Center for Excellence in Regional Atmospheric Environment, Chinese
Academy of Science, Xiamen, 361021, China
Viewed
Total article views: 4,285 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,047
1,135
103
4,285
486
117
180
HTML: 3,047
PDF: 1,135
XML: 103
Total: 4,285
Supplement: 486
BibTeX: 117
EndNote: 180
Views and downloads (calculated since 20 May 2019)
Cumulative views and downloads
(calculated since 20 May 2019)
Total article views: 3,438 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,605
743
90
3,438
254
99
160
HTML: 2,605
PDF: 743
XML: 90
Total: 3,438
Supplement: 254
BibTeX: 99
EndNote: 160
Views and downloads (calculated since 14 May 2020)
Cumulative views and downloads
(calculated since 14 May 2020)
Total article views: 847 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
442
392
13
847
232
18
20
HTML: 442
PDF: 392
XML: 13
Total: 847
Supplement: 232
BibTeX: 18
EndNote: 20
Views and downloads (calculated since 20 May 2019)
Cumulative views and downloads
(calculated since 20 May 2019)
Viewed (geographical distribution)
Total article views: 4,285 (including HTML, PDF, and XML)
Thereof 4,143 with geography defined
and 142 with unknown origin.
Total article views: 3,438 (including HTML, PDF, and XML)
Thereof 3,401 with geography defined
and 37 with unknown origin.
Total article views: 847 (including HTML, PDF, and XML)
Thereof 742 with geography defined
and 105 with unknown origin.
The bare black carbon (BC) was in a fractal structure. With coating thickness increasing, BC changed from a fractal structure to a core–shell structure. In the ambient atmosphere, plenty of BC particles were not in a perfect core–shell structure. This study brought attention to the combined effects of morphology and coating thickness on the absorption enhancement of BC-containing particles, which is helpful for determining the climatic effects of BC.
The bare black carbon (BC) was in a fractal structure. With coating thickness increasing, BC...
