Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon
文献类型：期刊论文
| 作者 | He,B(He,Bian)1,2; He,Bian |
| 刊名 | Theoretical and Applied Climatology
 |
| 出版日期 | 2017-05 |
| 卷号 | 128期号:3-4页码:905-917 |
| 关键词 | Tibetan Plateau asian Summer Monsoon East Asian Summer Monsoon diabatic Heating monsoon Precipitation |
| DOI | 10.1007/s00704-016-1746-5 |
| 文献子类 | 期刊论文 |
| 英文摘要 | Based on a series of topographical and thermal sensitivity experiments, the physical processes on the changes of Asian summer monsoon caused by the Himalaya elevated heating were investigated. Six different Himalaya–Iranian Plateau mountain heights were used: 0, 20, 40, 60, 80, and 100 % in the first group (called HIM). The no sensible heating experiments (called HIM_NS) were also performed with the same six mountain heights, but the surface sensible heating was not allowed to heat the atmosphere. The results indicate that the elevated heating effect of the Himalaya gradually intensified when the Himalaya uplifts. The establishment of SASM over the South Asian land which is characterized by the strong precipitation over south slope of the Tibetan Plateau and the huge warm anticyclone in the upper troposphere are in proportion to the elevated heating effect of the Himalaya. Further analysis suggests that the surface heat fluxes over the Himalaya keep almost unchanged during the uplifting, but the lifted condensation level reduces gradually over the regions where the mountain uplifts. The condensation moisturing increases correspondingly and leads to the increase of latent heating in the upper troposphere. Therefore, the positive feedback between the moist convection over the south slope of the Himalaya and monsoon circulation over Indian subcontinent forms and the successive precipitation over the South Asian land is maintained. |
| 项目编号 | GYHY201406001 ; 2014CB953904 ; 41405091 ; 91337110 ; SKLLQG1216 ; XDA11010402 |
| 语种 | 英语 |
| 资助机构 | ChinaMeteorological Administration ; ChinaMeteorological Administration ; NationalKey Basic Research Program of China ; NationalKey Basic Research Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; State Key Laboratory of Loess and Quaternary Geology ; State Key Laboratory of Loess and Quaternary Geology ; Strategic Leading Science Projects of theChinese Academy of Sciences ; Strategic Leading Science Projects of theChinese Academy of Sciences |
| 源URL | [http://ir.ieecas.cn/handle/361006/5603]  |
| 专题 | 地球环境研究所_黄土与第四纪地质国家重点实验室（2010~） |
| 通讯作者 | He,Bian |
| 作者单位 | 1.State Key Laboratory of Numerical Modeling for AtmosphericSciences and Geophysical Fluid Dynamics, Institute of AtmosphericPhysics, Chinese Academy of Sciences, Beijing 100029, China 2.State Key Laboratory of Loess and Quaternary Geology, Institute ofEarth Environment, Chinese Academy of Sciences, Xi’an 710075,China |
| 推荐引用方式 GB/T 7714 | He,B,He,Bian. Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon[J]. Theoretical and Applied Climatology,2017,128(3-4):905-917. |
| APA | He,B,&He,Bian.(2017).Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon.Theoretical and Applied Climatology,128(3-4),905-917. |
| MLA | He,B,et al."Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon".Theoretical and Applied Climatology 128.3-4(2017):905-917. |
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。