Simulated Impact of the Tibetan Glacier Expansion on the Eurasian Climate and Glacial Surface Mass Balance during the Last Glacial Maximum
文献类型：期刊论文
| 作者 | Liu, Yonggang1; Wu, Yubin2; Lin, Zhongda3; Zhang, Yang4; Zhu, Jiang5; Yi, Chaolu6 |
| 刊名 | JOURNAL OF CLIMATE
 |
| 出版日期 | 2020-08-01 |
| 卷号 | 33期号:15页码:6491-6509 |
| ISSN号 | 0894-8755 |
| DOI | 10.1175/JCLI-D-19-0763.1 |
| 通讯作者 | Yi, Chaolu(clyi@itpcas.ac.cn) |
| 英文摘要 | Glaciers over the Tibetan Plateau and surrounding regions during the Last Glacial Maximum (LGM) were much more extensive than during the preindustrial period (PI). The climate impact of such glacial expansion is studied here using the Community Atmosphere Model, version 4 (CAM4). To cover the range of uncertainty in glacier area during the LGM, the following three values are tested: 0.35 x 10(6), 0.53 x 10(6), and 0.70 x 10(6) km(2). The added glacier is distributed approximately equally over the Pamir region and the Himalayas. If 0.70 x 10(6) km(2) is used, the annual mean surface temperature of the glaciated regions would be cooled by similar to 3.5 degrees C. The annual mean precipitation would be reduced by 0.2 mm day(-1) (10%) and 2.5 mm day(-1) (24%) over the Pamir region and Himalayas, respectively. The surface mass balance (SMB) of the glaciers changes by 0.55 m yr(-1) (280%) and 20.32 m yr(-1) (220%) over the two regions, respectively. The changes in SMB remain large (0.29 and 20.13 m yr(-1)), even if the area of the Tibetan glacier were 0.35x10(6) km(2). Therefore, based on the results of this particular model, the expansion of glaciers can either enhance or slow the glacial growth. Moreover, the expansion of glaciers over the Himalayas reduces summer precipitation in central and northern China by similar to 0.5 mm day(-1) and increases summer precipitation in southern Asia by similar to 0.6 mm day(-1). The expansion of glaciers over the Pamir region has a negligible influence on the precipitation in these monsoonal regions, which is likely due to its large distance from the main monsoonal regions. |
| 资助项目 | National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41630527] ; National Natural Science Foundation of China[41230523] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA20070102] |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| 出版者 | AMER METEOROLOGICAL SOC |
| WOS记录号 | WOS:000615097400011 |
| 资助机构 | National Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences |
| 源URL | [http://ir.ieecas.cn/handle/361006/15916]  |
| 专题 | 地球环境研究所_加速器质谱中心 |
| 通讯作者 | Yi, Chaolu |
| 作者单位 | 1.Peking Univ, Dept Atmospher & Ocean Sci, Beijing, Peoples R China 2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Ge, Beijing, Peoples R China 4.Nanjing Univ, Sch Atmospher Sci, Nanjing, Peoples R China 5.Univ Michigan, Dept Earth & Environm Sci, Ann Arbor, MI 48109 USA 6.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu, Yonggang,Wu, Yubin,Lin, Zhongda,et al. Simulated Impact of the Tibetan Glacier Expansion on the Eurasian Climate and Glacial Surface Mass Balance during the Last Glacial Maximum[J]. JOURNAL OF CLIMATE,2020,33(15):6491-6509. |
| APA | Liu, Yonggang,Wu, Yubin,Lin, Zhongda,Zhang, Yang,Zhu, Jiang,&Yi, Chaolu.(2020).Simulated Impact of the Tibetan Glacier Expansion on the Eurasian Climate and Glacial Surface Mass Balance during the Last Glacial Maximum.JOURNAL OF CLIMATE,33(15),6491-6509. |
| MLA | Liu, Yonggang,et al."Simulated Impact of the Tibetan Glacier Expansion on the Eurasian Climate and Glacial Surface Mass Balance during the Last Glacial Maximum".JOURNAL OF CLIMATE 33.15(2020):6491-6509. |
入库方式： OAI收割
来源：地球环境研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。