Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon

doi:10.1007/s00704-016-1746-5

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（2010~）

	Influences of elevated heating effect by the Himalayaon the changes in Asian summer monsoon
	He,B(He,Bian)1,2; He,Bian
	2017-05
发表期刊	Theoretical and Applied Climatology
卷号	128 期号:3-4 页码:905-917
文章类型	期刊论文
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.
关键词	Tibetan Plateau asian Summer Monsoon East Asian Summer Monsoon diabatic Heating monsoon Precipitation
DOI	10.1007/s00704-016-1746-5
收录类别	SCI
所属项目编号	GYHY201406001 ; 2014CB953904 ; 41405091 ; 91337110 ; SKLLQG1216 ; XDA11010402
语种	英语
项目资助者	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
引用统计	被引频次：9[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/5603
专题	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
第一作者单位	黄土与第四纪地质国家重点实验室（1985-2004）
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.

条目包含的文件
文件名称/大小	文献类型	版本类型	开放类型	使用许可
Influences of elevat（5904KB）	期刊论文	出版稿	开放获取	CC BY-NC-SA	请求全文