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 |
卷 | 61 |
期 | 3-4 |
页 | 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
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