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: 4,341 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,750
1,430
161
4,341
136
218
HTML: 2,750
PDF: 1,430
XML: 161
Total: 4,341
BibTeX: 136
EndNote: 218
Views and downloads (calculated since 03 Apr 2017)
Cumulative views and downloads
(calculated since 03 Apr 2017)
Total article views: 3,483 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
2,268
1,100
115
3,483
115
162
HTML: 2,268
PDF: 1,100
XML: 115
Total: 3,483
BibTeX: 115
EndNote: 162
Views and downloads (calculated since 09 Oct 2017)
Cumulative views and downloads
(calculated since 09 Oct 2017)
Total article views: 858 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
482
330
46
858
21
56
HTML: 482
PDF: 330
XML: 46
Total: 858
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: 4,341 (including HTML, PDF, and XML)
Thereof 4,327 with geography defined
and 14 with unknown origin.
Total article views: 3,483 (including HTML, PDF, and XML)
Thereof 3,483 with geography defined
and 0 with unknown origin.
Total article views: 858 (including HTML, PDF, and XML)
Thereof 832 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...