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DOI	10.5194/hess-8-115-2004
	The origin of summer monsoon rainfall at New Delhi by deuterium excess
	Pang, HX; He, YQ; Zhang, ZL; Lu, AG; Gu, J
发表日期	2004
ISSN	1027-5606
EISSN	1607-7938
起始页码	115
结束页码	118
卷号	8 期号:1
英文摘要	The deuterium excess in summer monsoon precipitation, determined from isotopic measurements (delta(18)O and deltaD) at New Delhi, has been shorn to be correlated, negatively, with relative humidity at the 1000 hPa level over the western Arabian Sea. Furthermore, summer rainfall in north-western India is correlated. positively, with the zonal wind speed at the 1000 hPa level over the western Arabian Sea. while relative humidity is correlated, negatively, with zonal wind speed at the same level. It is concluded that evaporation from the western Arabian Sea is a major source of the summer rainfall at New Delhi.
关键词	PRECIPITATION INDIA
英文关键词	deuterium excess; relative humidity; origin of precipitation
语种	英语
WOS研究方向	Geology ; Water Resources
WOS类目	Geosciences, Multidisciplinary ; Water Resources
WOS记录号	WOS:000221788300013
来源期刊	HYDROLOGY AND EARTH SYSTEM SCIENCES
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/257351
推荐引用方式 GB/T 7714	Pang, HX,He, YQ,Zhang, ZL,et al. The origin of summer monsoon rainfall at New Delhi by deuterium excess[J]. 中国科学院青藏高原研究所,2004,8(1).
APA	Pang, HX,He, YQ,Zhang, ZL,Lu, AG,&Gu, J.(2004).The origin of summer monsoon rainfall at New Delhi by deuterium excess.HYDROLOGY AND EARTH SYSTEM SCIENCES,8(1).
MLA	Pang, HX,et al."The origin of summer monsoon rainfall at New Delhi by deuterium excess".HYDROLOGY AND EARTH SYSTEM SCIENCES 8.1(2004).