Climate Change Data Portal
DOI | 10.1007/s00382-016-3133-4 |
Abundant climatic information in water stable isotope record from a maritime glacier on southeastern Tibetan Plateau | |
Zhao, Huabiao; Xu, Baiqing; Li, Zhen; Wang, Mo; Li, Jiule; Zhang, Xiaolong | |
通讯作者 | Zhao, HB (通讯作者) |
发表日期 | 2017 |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
起始页码 | 1161 |
结束页码 | 1171 |
卷号 | 48期号:3-4 |
英文摘要 | Climatic significance of ice core stable isotope record in the Himalayas and southern Tibetan Plateau (TP), where the climate is alternately influenced by Indian summer monsoon and mid-latitude westerlies, is still debated. A newly drilled Zuoqiupu ice core from a temperate maritime glacier on the southeastern TP covering 1942-2011 is investigated in terms of the relationships between delta O-18 and climate parameters. Distinct seasonal variation of delta O-18 is observed due to high precipitation amount in this area. Thus the monsoon (June to September) and non-monsoon (October to May) delta O-18 records are reconstructed, respectively. The temperature effect is identified in the annual delta O-18 record, which is predominantly contributed by temperature control on the non-monsoon precipitation delta O-18 record. Conversely, the negative correlation between annual delta O-18 record and precipitation amount over part of Northeast India is mostly contributed by the monsoon precipitation delta O-18 record. The variation of monsoon delta O-18 record is greatly impacted by the Indian summer monsoon strength, while that of non-monsoon delta O-18 record is potentially associated with the mid-latitude westerly activity. The relationship between Zuoqiupu delta O-18 record and Sea Surface Temperature (SST) is found to be inconsistent before and after the climate shift of 1976/1977. In summer monsoon season, the role of SST in the monsoon delta O-18 record is more important in eastern equatorial Pacific Ocean and tropical Indian Ocean before and after the shift, respectively. In non-monsoon season, however, the Atlantic Multidecadal Oscillation has a negative impact before but positive impact after the climate shift on the non-monsoon delta O-18 record. |
关键词 | ICE CORESUMMER MONSOONASIAN MONSOONINDIAN MONSOONPRECIPITATIONSOUTHVARIABILITYENSOOSCILLATIONRAINFALL |
英文关键词 | Ice core; Maritime glacier; Stable isotope record; Indian summer monsoon; Westerly |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000394150500026 |
来源期刊 | CLIMATE DYNAMICS
![]() |
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/258885 |
推荐引用方式 GB/T 7714 | Zhao, Huabiao,Xu, Baiqing,Li, Zhen,et al. Abundant climatic information in water stable isotope record from a maritime glacier on southeastern Tibetan Plateau[J]. 中国科学院青藏高原研究所,2017,48(3-4). |
APA | Zhao, Huabiao,Xu, Baiqing,Li, Zhen,Wang, Mo,Li, Jiule,&Zhang, Xiaolong.(2017).Abundant climatic information in water stable isotope record from a maritime glacier on southeastern Tibetan Plateau.CLIMATE DYNAMICS,48(3-4). |
MLA | Zhao, Huabiao,et al."Abundant climatic information in water stable isotope record from a maritime glacier on southeastern Tibetan Plateau".CLIMATE DYNAMICS 48.3-4(2017). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。