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DOI10.1360/982005-802
Isotopic composition of atmospheric water vapor before and after the monsoon's end in the Nagqu River Basin
Yu, WS; Yao, TD; Tian, LD; Wang, Y; Wusheng, Y
发表日期2005
ISSN1001-6538
EISSN1861-9541
起始页码2755
结束页码2760
卷号50期号:23
英文摘要Atmospheric water vapor samples were collected in the Nagqu River Basin in the middle of Tibetan Plateau between August and October in 2004. Results show that there exist some fluctuations of the delta O-18 of atmospheric water vapor, especially before and after the monsoon's end. Moreover, the variety trend of the delta O-18 of atmospheric water vapor inverse correlates with that of dew point. Precipitation events make an important effect upon the variation of delta O-18 of atmospheric water vapor. During the whole sampling period, the delta O-18 values of atmospheric water vapor are low while precipitation events occurred. The moisture origins also contribute to the variation of delta O-18 of atmospheric water vapor. The oceanic moisture transported by the southwest monsoon results in lower delta O-18 of atmospheric water vapor in the Nagqu River Basin. Compared with the influence of the oceanic moisture, the delta O-18 values, however, appear high resulting from the effect of the continental air mass in this region.
关键词TIBETAN PLATEAUICE-COREPRECIPITATIONTEMPERATUREDELTA-O-18MOISTURERATIOSRECORDO-18
英文关键词Nagqu River Basin; delta O-18; atmospheric water vapor
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000235457300015
来源期刊CHINESE SCIENCE BULLETIN
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/257369
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GB/T 7714
Yu, WS,Yao, TD,Tian, LD,et al. Isotopic composition of atmospheric water vapor before and after the monsoon's end in the Nagqu River Basin[J]. 中国科学院青藏高原研究所,2005,50(23).
APA Yu, WS,Yao, TD,Tian, LD,Wang, Y,&Wusheng, Y.(2005).Isotopic composition of atmospheric water vapor before and after the monsoon's end in the Nagqu River Basin.CHINESE SCIENCE BULLETIN,50(23).
MLA Yu, WS,et al."Isotopic composition of atmospheric water vapor before and after the monsoon's end in the Nagqu River Basin".CHINESE SCIENCE BULLETIN 50.23(2005).
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