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DOI10.1360/982004-363
Origin of summer monsoon rainfall identified by delta O-18 in precipitation
Pang, HX; He, YQ; Zhang, ZL; Lu, AG; Gu, J; Zhao, JD
发表日期2005
ISSN1001-6538
EISSN1861-9541
起始页码2761
结束页码2764
卷号50期号:23
英文摘要A negative correlation between delta O-18 in monsoon precipitation and f, the ratio of precipitable water in monsoon region to that in water source area, is hypothesized. Using the Rayleigh model, a new method for identifying origin of summer monsoon rainfall is developed based on the hypothesis. In order to validate the method, the isotopic data at New Delhi, a typical station in the southwest monsoon region, and Hong Kong, a typical station in the southeast monsoon region, were collected and analyzed for case studies. The case studies indicate that the water source areas of the monsoon rainfall at the two stations identified by the method are accordant with the general atmosphere circulation patterns. The method developed in this paper is significantly important for tracing the origin of summer monsoon precipitation.
关键词TIBETAN PLATEAUINTERANNUAL VARIABILITYDEUTERIUM EXCESSSTABLE ISOTOPESWATERMODELO-18SNOW
英文关键词monsoon; stable isotopes; origin of monsoon precipitation
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000235457300016
来源期刊CHINESE SCIENCE BULLETIN (IF:1.649[JCR-2016],1.738[5-Year])
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/257368
推荐引用方式
GB/T 7714
Pang, HX,He, YQ,Zhang, ZL,et al. Origin of summer monsoon rainfall identified by delta O-18 in precipitation[J]. 中国科学院青藏高原研究所,2005,50(23).
APA Pang, HX,He, YQ,Zhang, ZL,Lu, AG,Gu, J,&Zhao, JD.(2005).Origin of summer monsoon rainfall identified by delta O-18 in precipitation.CHINESE SCIENCE BULLETIN,50(23).
MLA Pang, HX,et al."Origin of summer monsoon rainfall identified by delta O-18 in precipitation".CHINESE SCIENCE BULLETIN 50.23(2005).
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