Modeling the Origin of Anthropogenic Black Carbon and Its Climatic Effect Over the Tibetan Plateau and Surrounding Regions
文献类型：期刊论文
| 作者 | Yang, Junhua1; Kang, Shichang1,2; Ji, Zhenming3,4; Chen, Deliang5 |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
 |
| 出版日期 | 2018-01-27 |
| 卷号 | 123期号:2页码:671-692 |
| 关键词 | black carbon emission origin Tibetan Plateau South Asia transport process |
| ISSN号 | 2169-897X |
| DOI | 10.1002/2017JD027282 |
| 通讯作者 | Kang, Shichang(shichang.kang@lzb.ac.cn) ; Ji, Zhenming(jizhm3@mail.sysu.edu.cn) |
| 英文摘要 | Black carbon (BC) in snow/ice induces enhanced snow and glacier melting. As over 60% of atmospheric BC is emitted from anthropogenic sources, which directly impacts the distribution and concentration of BC in snow/ice, it is essential to assess the origin of anthropogenic BC transported to the Tibetan Plateau (TP) where there are few direct emissions attributable to local human activities. In this study, we used a regional climate-atmospheric chemistry model and a set of BC scenarios for quantitative evaluation of the impact of anthropogenic BC from various sources and its climate effects over the TP in 2013. The results showed that the model performed well in terms of climatology, aerosol optical properties, and near-surface concentrations, which indicates that this modeling framework is appropriate to characterize anthropogenic BC source-receptor relationships over the TP. The simulated surface concentration associated with the anthropogenic sources showed seasonal differences. In the monsoon season, the contribution of anthropogenic BC was less than in the nonmonsoon season. In the nonmonsoon season, westerly winds prevailed and transported BC from central Asia and north India to the western TP. In the monsoon season, BC aerosol was transported to the middle-upper troposphere over the Indo-Gangetic Plain and crossed the Himalayas via southwesterly winds. The majority of anthropogenic BC over the TP was transported from South Asia, which contributed to 40%-80% (mean of 61.3%) of surface BC in the nonmonsoon season, and 10%-50% (mean of 19.4%) in the monsoon season. For the northeastern TP, anthropogenic BC from eastern China accounted for less than 10% of the total in the nonmonsoon season but can be up to 50% in the monsoon season. Averaged over the TP, the eastern China anthropogenic sources accounted for 6.2% and 8.4% of surface BC in the nonmonsoon and monsoon seasons, respectively. The anthropogenic BC induced negative radiative forcing and cooling effects at the near surface over the TP. |
| 收录类别 | SCI |
| WOS关键词 | LIGHT-ABSORBING IMPURITIES ; ASIAN SUMMER MONSOON ; SNOW COVER ; OPTICAL-PROPERTIES ; WESTERN CHINA ; NORTH CHINA ; WRF MODEL ; AEROSOL ; ICE ; EMISSIONS |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS类目 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000425520200003 |
| 出版者 | AMER GEOPHYSICAL UNION |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2558087 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Kang, Shichang; Ji, Zhenming |
| 作者单位 | 1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou, Gansu, Peoples R China 2.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 3.Sun Yat Sen Univ, Sch Atmospher Sci, Guangzhou, Guangdong, Peoples R China 4.Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou, Guangdong, Peoples R China 5.Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden |
| 推荐引用方式 GB/T 7714 | Yang, Junhua,Kang, Shichang,Ji, Zhenming,et al. Modeling the Origin of Anthropogenic Black Carbon and Its Climatic Effect Over the Tibetan Plateau and Surrounding Regions[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(2):671-692. |
| APA | Yang, Junhua,Kang, Shichang,Ji, Zhenming,&Chen, Deliang.(2018).Modeling the Origin of Anthropogenic Black Carbon and Its Climatic Effect Over the Tibetan Plateau and Surrounding Regions.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(2),671-692. |
| MLA | Yang, Junhua,et al."Modeling the Origin of Anthropogenic Black Carbon and Its Climatic Effect Over the Tibetan Plateau and Surrounding Regions".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.2(2018):671-692. |
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来源：寒区旱区环境与工程研究所
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