Key Laboratory of Tibetan Environment Changes and Land
Surface Processes, Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
Laboratory of Green Chemistry, Lappeenranta University of
Technology, Sammonkatu 12, 50130 Mikkeli, Finland
CAS Center for Excellence in Tibetan Plateau Earth Sciences,
Beijing 100101, China
Fangping Yan
Laboratory of Green Chemistry, Lappeenranta University of
Technology, Sammonkatu 12, 50130 Mikkeli, Finland
Shichang Kang
State Key Laboratory of Cryospheric Sciences, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of
Sciences, Lanzhou 730000, China
CAS Center for Excellence in Tibetan Plateau Earth Sciences,
Beijing 100101, China
Pengfei Chen
State Key Laboratory of Cryospheric Sciences, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of
Sciences, Lanzhou 730000, China
Xiaowen Han
Key Laboratory of Tibetan Environment Changes and Land
Surface Processes, Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
University of Chinese Academy of Sciences, Beijing 100049,
China
Zhaofu Hu
State Key Laboratory of Cryospheric Sciences, Northwest
Institute of Eco-Environment and Resources, Chinese Academy of
Sciences, Lanzhou 730000, China
University of Chinese Academy of Sciences, Beijing 100049,
China
Guoshuai Zhang
Key Laboratory of Tibetan Environment Changes and Land
Surface Processes, Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
Ye Hong
Institute of Atmospheric Environment, China Meteorological
Administration, Shenyang 110166, China
Shaopeng Gao
Key Laboratory of Tibetan Environment Changes and Land
Surface Processes, Institute of Tibetan Plateau Research, Chinese
Academy of Sciences, Beijing 100101, China
Bin Qu
Laboratory of Green Chemistry, Lappeenranta University of
Technology, Sammonkatu 12, 50130 Mikkeli, Finland
Zhejing Zhu
Environmental Research Institute, Shandong University, Jinan
250100, China
Jiwei Li
Environmental Research Institute, Shandong University, Jinan
250100, China
Bing Chen
Environmental Research Institute, Shandong University, Jinan
250100, China
Mika Sillanpää
Laboratory of Green Chemistry, Lappeenranta University of
Technology, Sammonkatu 12, 50130 Mikkeli, Finland
Department of Civil and Environmental Engineering, Florida
International University, Miami, FL 33174, USA
Viewed
Total article views: 4,415 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,786
1,463
166
4,415
141
225
HTML: 2,786
PDF: 1,463
XML: 166
Total: 4,415
BibTeX: 141
EndNote: 225
Views and downloads (calculated since 03 Apr 2017)
Cumulative views and downloads
(calculated since 03 Apr 2017)
Total article views: 3,550 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,303
1,127
120
3,550
120
169
HTML: 2,303
PDF: 1,127
XML: 120
Total: 3,550
BibTeX: 120
EndNote: 169
Views and downloads (calculated since 09 Oct 2017)
Cumulative views and downloads
(calculated since 09 Oct 2017)
Total article views: 865 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
483
336
46
865
21
56
HTML: 483
PDF: 336
XML: 46
Total: 865
BibTeX: 21
EndNote: 56
Views and downloads (calculated since 03 Apr 2017)
Cumulative views and downloads
(calculated since 03 Apr 2017)
Viewed (geographical distribution)
Total article views: 4,415 (including HTML, PDF, and XML)
Thereof 4,401 with geography defined
and 14 with unknown origin.
Total article views: 3,550 (including HTML, PDF, and XML)
Thereof 3,550 with geography defined
and 0 with unknown origin.
Total article views: 865 (including HTML, PDF, and XML)
Thereof 839 with geography defined
and 26 with unknown origin.
In this study, we found, due to contribution of carbonates, previously reported BC concentration in atmosphere of the Himalayas and Tibetan Plateau (HTP) were overestimated by around 39–52 %. Meanwhile, we found BC deposition of lake cores overestimated the atmospheric deposition of BC in the HTP; BC depositions of glacier region reflected actual values of 17.9 ± 5.3 mg m−2 a−1. The above results are critical for studying atmospheric distribution and chemical transport of BC in and around the HTP.
In this study, we found, due to contribution of carbonates, previously reported BC concentration...
