Precipitation stable isotope records from the northern Hengduan Mountains in China capture signals of the winter India-Burma Trough and the Indian Summer Monsoon
文献类型：期刊论文
| 作者 | Ma, YM (Ma, Yaoming)1,2; Yu, WS (Yu, Wusheng)1,2; Tian, LD (Tian, Lide)1,2,3; Yao, TD (Yao, Tandong)1,2; Xu, BQ (Xu, Baiqing)1,2; Wei, FL (Wei, Feili)1,2,4; Zhu, HF (Zhu, Haifeng)1,2; Luo, L (Luo, Lun)2; Qu, DM (Qu, Dongmei)2; Yu, WS |
| 刊名 | EARTH AND PLANETARY SCIENCE LETTERS
 |
| 出版日期 | 2017 |
| 卷号 | 477期号:0页码:123-133 |
| 关键词 | Southeastern Tibetan Plateau Ice Cores Meteorological Factors Climatic Sensitivity Maritime Glacier Southwest China Oxygen Isotopes Water Delta-o-18 Vapor |
| DOI | 10.1016/j.epsl.2017.08.018 |
| 文献子类 | Article |
| 英文摘要 | This project reports results of the first precipitation stable isotope (delta O-18 and delta D) time series produced for Qamdo in the northern Hengduan Mountains in the southeastern Tibetan Plateau. The data showed that the fluctuations of precipitation stable isotopes at Qamdo during the different seasons revealed various moisture sources. The westerlies and local recycling moisture dominated at the study area before the pre-monsoon and after the post-monsoon seasons, which resulted in similar trends of both precipitation stable isotopes and temperature. The marine moisture was transported to the northern Hengduan Mountains by the winter India-Burma Trough combined with convection. Consequently, stable isotopes in subsequent precipitation were occasionally observed to decrease suddenly. However, delta O-18 and delta D values of precipitation at Qamdo were lower during the monsoon period and the duration of those low values was longer because of the effects of the Indian Summer Monsoon and the strengthening convection. Our findings indicate that the effects of seasonal precipitation differences caused by various climate systems, including the winter India-Burma Trough and Indian Summer Monsoon, need to be considered when attempting to interpret tree-ring and ice core records for the Hengduan Mountains. (C) 2017 Elsevier B.V. All rights reserved. |
| 学科主题 | 自然地理学 |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000413132000012 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/7956]  |
| 专题 | 青藏高原研究所_图书馆 |
| 通讯作者 | Yu, WS |
| 作者单位 | 1.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China. 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China. 3.Yunnan Univ, Inst Int Rivers & Ecosecur, Kunming 650091, Yunnan, Peoples R China. 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China. |
| 推荐引用方式 GB/T 7714 | Ma, YM ,Yu, WS ,Tian, LD ,et al. Precipitation stable isotope records from the northern Hengduan Mountains in China capture signals of the winter India-Burma Trough and the Indian Summer Monsoon[J]. EARTH AND PLANETARY SCIENCE LETTERS,2017,477(0):123-133. |
| APA | Ma, YM .,Yu, WS .,Tian, LD .,Yao, TD .,Xu, BQ .,...&Yu, WS.(2017).Precipitation stable isotope records from the northern Hengduan Mountains in China capture signals of the winter India-Burma Trough and the Indian Summer Monsoon.EARTH AND PLANETARY SCIENCE LETTERS,477(0),123-133. |
| MLA | Ma, YM ,et al."Precipitation stable isotope records from the northern Hengduan Mountains in China capture signals of the winter India-Burma Trough and the Indian Summer Monsoon".EARTH AND PLANETARY SCIENCE LETTERS 477.0(2017):123-133. |
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来源：青藏高原研究所
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