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: 4,024 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,875
1,067
82
4,024
424
98
145
HTML: 2,875
PDF: 1,067
XML: 82
Total: 4,024
Supplement: 424
BibTeX: 98
EndNote: 145
Views and downloads (calculated since 20 May 2019)
Cumulative views and downloads
(calculated since 20 May 2019)
Total article views: 3,199 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,436
692
71
3,199
227
83
132
HTML: 2,436
PDF: 692
XML: 71
Total: 3,199
Supplement: 227
BibTeX: 83
EndNote: 132
Views and downloads (calculated since 14 May 2020)
Cumulative views and downloads
(calculated since 14 May 2020)
Total article views: 825 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
439
375
11
825
197
15
13
HTML: 439
PDF: 375
XML: 11
Total: 825
Supplement: 197
BibTeX: 15
EndNote: 13
Views and downloads (calculated since 20 May 2019)
Cumulative views and downloads
(calculated since 20 May 2019)
Viewed (geographical distribution)
Total article views: 4,024 (including HTML, PDF, and XML)
Thereof 3,891 with geography defined
and 133 with unknown origin.
Total article views: 3,199 (including HTML, PDF, and XML)
Thereof 3,169 with geography defined
and 30 with unknown origin.
Total article views: 825 (including HTML, PDF, and XML)
Thereof 722 with geography defined
and 103 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...
