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Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence
Dittmar, T (Dittmar, Thorsten)8; Raymond, PA (Raymond, Peter A.)13; Li, CL (Li, Chaoliu)1,2,3; Chen, PF (Chen, Pengfei)4; Kang, SC (Kang, Shichang)2,4,5; Yan, FP (Yan, Fangping)3; Tripathee, L (Tripathee, Lekhendra)4; Wu, GJ (Wu, Guangjian)1,2; Qu, B (Qu, Bin)6; Sillanpaa, M (Sillanpaa, Mika)3
刊名JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
2018-06-16
卷号123期号:11页码:6248-6258  文献号 D028181
关键词LIGHT-ABSORPTION CHARACTERISTICS RESOLUTION MASS DATA ATMOSPHERIC AEROSOLS BLACK CARBON INORGANIC CARBON BROWN CLOUDS LHASA CITY MATTER DEPOSITION GLACIER
ISSN号2169-897X
DOI10.1029/2017JD028181
英文摘要The dissolved organic carbon in precipitation (water-soluble organic carbon, WSOC) can provide a carbon subsidy to receiving ecosystems. The concentrations, isotopic signatures (C-13/Delta C-14), and molecular signatures (transform ion cyclotron mass spectrometry) of WSOC being delivered to Nam Co-a remote site on the inland Tibetan Plateau (TP)were compared to those of WSOC in the snowpack, and in wet deposition from urban cities fringing the TP. The average WSOC concentration at Nam Co (1.0 +/- 0.9mg C L-1) was lower than for the large cities (1.6 to 2.3mgCL(-1)) but higher than in the snowpack samples (0.26 +/- 0.09mgCL(-1)). Based upon radiocarbon data, it is estimated that 156% of Nam Co WSOC was fossil derived, increasing to 208% for snowpack WSOC, 29 +/- 4% for Lhasa WSOC, and 34 +/- 8% for the three cities. Transform ion cyclotron mass spectrometry results revealed that the abundance of dissolved black carbon and sulfur-containing molecules of WSOC increased in the order Nam Co
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000436110800029
内容类型期刊论文
源URL[http://ir.itpcas.ac.cn/handle/131C11/8625]  
专题青藏高原研究所_图书馆
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China;
2.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;
3.Lappeenranta Univ Technol, Lab Green Chem, Mikkeli, Finland;
4.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou, Gansu, Peoples R China;
5.Univ CAS, Beijing, Peoples R China;
6.Nanjing Univ Informat Sci & Technol, Int Joint Lab Climate & Environm Change, Yale NUIST Ctr Atmospher Environm, Nanjing, Jiangsu, Peoples R China;
7.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu, Sichuan, Peoples R China;
8.Carl Von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm, ICBM MPI Bridging Grp, Res Grp Marine Geochem, Oldenburg, Germany;
9.Northeastern Univ, Dept Marine Sci, Boston, MA 02115 USA;
10.Northeastern Univ, Dept Environm Sci, Boston, MA 02115 USA;
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Dittmar, T ,Raymond, PA ,Li, CL ,et al. Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(11):6248-6258  文献号 D028181.
APA Dittmar, T .,Raymond, PA .,Li, CL .,Chen, PF .,Kang, SC .,...&Stubbins, A .(2018).Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(11),6248-6258  文献号 D028181.
MLA Dittmar, T ,et al."Fossil Fuel Combustion Emission From South Asia Influences Precipitation Dissolved Organic Carbon Reaching the Remote Tibetan Plateau: Isotopic and Molecular Evidence".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.11(2018):6248-6258  文献号 D028181.
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