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《Chinese Science Bulletin》 2009-06
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Spatial distribution of δ~(18)O in precipitation over China

LIU ZhongFang1,2, TIAN LiDe2,3, YAO TanDong2,3 & CHAI XuRong4 1 Tianjin Key Laboratory of Water Environment and Water Resource, Tianjin Normal University, Tianjin 300387, China; 2 Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China; 3 The State Key Laboratory of Cryosphere Sciences, Lanzhou 730000, China; 4 College of Urban and Environment Science, Shanxi Normal University, Linfen 041004, China  
Studies have shown that the variation of δ 18O in precipitation is closely linked to the thermodynam- ics of water vapor condensation during Rayleigh distillation. The water vapor condensation is mainly controlled by low temperature as a result of increasing altitude or latitude. The BW model, established by Bowen and Wilkinson, demonstrated that δ18O in precipitation can be modeled ac- curately as a function of latitude and altitude, which can estimate the isotopic composition in the absence of more data. Based on BW model, this paper established a model of the quantitative rela- tionship between δ18O in precipitation and latitude and altitude using the existing δ18O data from 55 sites across China. The model was described as δ18Oppt=-0.0176LAT2 + 1.1195LAT-0.0016ALT-23.7553. According to this model, a higher-resolution map of mean annual δ18O for precipitation across China has been generated using geographic information system software, integrating with latitude, altitude as well as moisture cycle. Spatial distribution of δ18O in modern precipitation of China is revealed from a new approach, which provides important information for the study on an- cient climate and stable isotopic hydrology.
【Fund】: 国家自然科学基金(批准号:40771048 40571039);; 天津市科技发展计划(批准号:06YFSZSF05100)资助项目
【CateGory Index】: P426.612
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