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DOI | 10.1016/j.epsl.2019.115837 |
Indian monsoon precipitation isotopes linked with high level cloud cover at local and regional scales | |
Wang, Di; Tian, Lide; Cai, Zhongyin; Shao, Lili; Guo, Xiaoyu; Tian, Ran; Li, Yike; Chen, Yiliang; Yuan, Chuan | |
通讯作者 | Tian, LD (通讯作者) |
发表日期 | 2020 |
ISSN | 0012-821X |
EISSN | 1385-013X |
卷号 | 529 |
英文摘要 | Precipitation stable isotopes preserve historic changes of evaporation in the source regions and precipitation processes, therefore, they can be used to reveal regional hydrological cycle dynamics and paleoclimate reconstructions. In monsoon regions, strong inverse impacts of convection on precipitation isotope ratios, have created a debate regarding the interpretation of isotope records as local climate proxies. The proportions of stratiform to convective precipitation on water isotopes, together with the influence mechanisms on seasonal and interannual scales remain highly uncertain. To further address the influence of precipitation patterns on water isotopes, we used 10 yrs of precipitation isotope data from the southern Tibetan Plateau (TP) to explore the effects of large-scale cloud cover and local climate on precipitation isotopes. Correlation analysis performed between local precipitation delta O-18 values and different level cloud data, indicated significant negative correlations between precipitation isotopes and high level cloud cover on both seasonal and interannual time scales. This result suggests that high-level convection in the upper moisture transport stream is a main control on precipitation isotopes in the southern TP. The clear and coherent variations of precipitation isotopes with the Southern Oscillation Index and outgoing longwave radiation confirmed that strong convection activity in the moisture source region and during transport significantly depleted heavy isotopes in vapor, producing substantially decreased precipitation delta O-18 in the study region. These results agree with earlier findings of tree ring cellulose isotope records that correlate with cloud cover, but we emphasized the important role of larger-scale regional cloud cover. We also delineated different maximum correlation zones for seasonal and interannual time scales, likely due to different mechanisms. These findings further improve the interpretation of paleoisotope records from the Indian summer monsoon region. (C) 2019 Elsevier B.V. All rights reserved. |
关键词 | TIBETAN PLATEAUSTABLE-ISOTOPESASIAN MONSOONINTERANNUAL VARIATIONSICE CORESVARIABILITYDELTA-O-18PATTERNSOXYGENSYSTEM |
英文关键词 | precipitation isotopes; cloud cover; convective activity; regional scale; southern Tibetan Plateau |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000496039600001 |
来源期刊 | EARTH AND PLANETARY SCIENCE LETTERS
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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/259817 |
推荐引用方式 GB/T 7714 | Wang, Di,Tian, Lide,Cai, Zhongyin,et al. Indian monsoon precipitation isotopes linked with high level cloud cover at local and regional scales[J]. 中国科学院青藏高原研究所,2020,529. |
APA | Wang, Di.,Tian, Lide.,Cai, Zhongyin.,Shao, Lili.,Guo, Xiaoyu.,...&Yuan, Chuan.(2020).Indian monsoon precipitation isotopes linked with high level cloud cover at local and regional scales.EARTH AND PLANETARY SCIENCE LETTERS,529. |
MLA | Wang, Di,et al."Indian monsoon precipitation isotopes linked with high level cloud cover at local and regional scales".EARTH AND PLANETARY SCIENCE LETTERS 529(2020). |
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