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DOI | 10.1007/s11430-011-4342-7 |
The Indian monsoonal influence on altitude effect of delta O-18 in surface water on southeast Tibetan Plateau | |
Yang XiaoXin; Xu BaiQing; Yang Wei; Qu DongMei | |
通讯作者 | Yang, XX (通讯作者) |
发表日期 | 2012 |
ISSN | 1674-7313 |
EISSN | 1869-1897 |
起始页码 | 438 |
结束页码 | 445 |
卷号 | 55期号:3 |
英文摘要 | The altitude effect of delta O-18 is essential for the study of the paleo-elevation reconstruction and possible to be solved through modern process studies. This study presents new delta O-18 results from southeast Tibetan Plateau along two transects, the Zayu transect and the Lhasa-Nyang transect, with delta O-18 data from June to September representative of monsoon period and delta O-18 data during the rest of the year of non-monsoon period. Altitude effect outweighs the longitude and latitude effects in determining regional delta O-18 variation spatially. Relevant delta O-18 data from previous studies in the nearby region have also been combined to comprehensively understand the influence of different moisture sources on delta O-18 from local scale to regional scale. The delta O-18 in surface water in the southeast Tibetan Plateau and its nearby regions influenced by the Indian summer monsoon shows that single dominant moisture source or simple moisture sources lead to smaller altitudinal lapse rate, whilst growing contributions from local convection to precipitation enlarge delta O-18-altitude rate. It thereupon reveals the significance of the Indian summer monsoon to the altitude effect of delta O-18 in surface water, and the complicated effect of local convection or westerlies evolution to the variation of altitudinal lapse rate. Paleo-monsoon evolution therefore should be considered when altitude effect is applied to paleo-elevation reconstruction for the Tibetan Plateau. |
关键词 | ISOTOPIC COMPOSITIONPRECIPITATION/RIVER WATERSTABLE ISOTOPESPALEOELEVATIONELEVATIONO-18HIMALAYABASINRIVERAREA |
英文关键词 | delta O-18; altitude effect; Indian monsoon; southeast Tibetan Plateau and its nearby regions; altitudinal lapse rate |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000302296800009 |
来源期刊 | SCIENCE CHINA-EARTH 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/257967 |
推荐引用方式 GB/T 7714 | Yang XiaoXin,Xu BaiQing,Yang Wei,et al. The Indian monsoonal influence on altitude effect of delta O-18 in surface water on southeast Tibetan Plateau[J]. 中国科学院青藏高原研究所,2012,55(3). |
APA | Yang XiaoXin,Xu BaiQing,Yang Wei,&Qu DongMei.(2012).The Indian monsoonal influence on altitude effect of delta O-18 in surface water on southeast Tibetan Plateau.SCIENCE CHINA-EARTH SCIENCES,55(3). |
MLA | Yang XiaoXin,et al."The Indian monsoonal influence on altitude effect of delta O-18 in surface water on southeast Tibetan Plateau".SCIENCE CHINA-EARTH SCIENCES 55.3(2012). |
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