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

doi:10.1007/s00704-016-1746-5

CORC > 地球环境研究所 > 中国科学院地球环境研究所 > 黄土与第四纪地质国家重点实验室（2010~）

	Influences of elevated heating effect by the Himalaya on the changes in Asian summer monsoon
	He, Bian 1,2
刊名	THEORETICAL AND APPLIED CLIMATOLOGY
	2017-05-01
卷号	128 期号:3-4 页码:905-917
DOI	10.1007/s00704-016-1746-5
文献子类	Article
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.
WOS关键词	LAND-SEA DISTRIBUTION ; TIBETAN PLATEAU ; MOUNTAIN UPLIFT ; SOUTH-ASIA ; GENERAL-CIRCULATION ; CLIMATE PATTERNS ; BOUNDARY-LAYER ; EAST-ASIA ; MODEL ; ATMOSPHERE
WOS研究方向	Meteorology & Atmospheric Sciences
语种	英语
WOS记录号	WOS:000399702200030
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/5482]
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~）
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 2.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	He, Bian. Influences of elevated heating effect by the Himalaya on the changes in Asian summer monsoon[J]. THEORETICAL AND APPLIED CLIMATOLOGY,2017,128(3-4):905-917.
APA	He, Bian.(2017).Influences of elevated heating effect by the Himalaya on the changes in Asian summer monsoon.THEORETICAL AND APPLIED CLIMATOLOGY,128(3-4),905-917.
MLA	He, Bian."Influences of elevated heating effect by the Himalaya on the changes in Asian summer monsoon".THEORETICAL AND APPLIED CLIMATOLOGY 128.3-4(2017):905-917.