中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau

文献类型:SCI/SSCI论文

作者Liang E. Y. ; Shao X. M. ; Qin N. S.
发表日期2008
关键词Tibetan Plateau dendroclimatology climate change historical climatic documents glacial fluctuations volcanic eruption ice cores precipitation variation air-temperature climate-change qinghai china delta-o-18 record forecast growth
英文摘要Understanding of past climatic variability over the Tibetan Plateau is still limited because of the lack of long-term climatic records. Here we reconstruct the mean summer (June-August) minimum temperature for the past 379 years based on tree-ring data in the source region of the Yangtze River. This reconstruction successfully captures recent abrupt climatic changes and agrees in general with other temperature reconstructions for the Tibetan Plateau on a decadal timescale. The cold and warm periods coincide with documented glacier advances and retreats on the east and southeast Tibetan Plateau. The interval 1816-22 is among the coldest periods in the reconstruction and may be related to the influence of the Tambora eruption in Indonesia in 1815. Comparisons with other paleoclimatic proxies imply a high degree of confidence for our reconstruction and its indicative power for a large-scale climate variability on the Tibetan Plateau. (c) 2007 Elsevier B.V. All rights reserved.
出处Global and Planetary Change
61
3-4
313-320
收录类别SCI
语种英语
ISSN号0921-8181
源URL[http://ir.igsnrr.ac.cn/handle/311030/23557]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Liang E. Y.,Shao X. M.,Qin N. S.. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. 2008.

入库方式: OAI收割

来源:地理科学与资源研究所

浏览0
下载0
收藏0
其他版本

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。