globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2015.01.003
论文题名:
Tree-ring density inferred late summer temperature variability over the past three centuries in the Gaoligong Mountains, southeastern Tibetan Plateau
作者: Li M.-Y.; Wang L.; Fan Z.-X.; Shen C.-C.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2015
卷: 422
起始页码: 57
结束页码: 64
语种: 英语
英文关键词: August-September temperature ; Larix speciosa ; Maximum latewood density ; Southeastern Tibetan Plateau ; Tree rings
英文摘要: Long and high-resolution proxy records are still sparse in the southeastern Tibetan Plateau (TP), hampering our understanding of past climatic variability from a long-term perspective. In this study, we developed a regional maximum latewood density (MXD) chronology of Larix speciosa stretching up to 523. years based on 72 tree-ring cores (44 trees) collected from three sites close to the tree line in the Gaoligong Mountains, southeastern TP. This chronology responded well to temperatures during August through September and was thus used to reconstruct late summer (August-September) temperature over the period A.D. 1690-2008. The reconstruction explains 40.9% of the total temperature variance during the calibration phase. Cold conditions prevailed during the periods 1695-1702, 1806-1821, the 1850s, 1882-1889, the 1900s and the 1960s. Warm phases occurred in 1734-1745, the 1770s, 1824-1840, the 1890s, 1927-1936, the 1940s-1950s and 2002-2008. Spatial correlation with the gridded temperature data set showed that our reconstruction captures large-scale regional temperature variations for the southeastern and southern TP. Comparison with other tree-ring inferred temperature time series in the surrounding areas, glacier fluctuations and historical documental records imply a high degree of confidence for our reconstruction. © 2015 Elsevier B.V.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/69019
Appears in Collections:过去全球变化的重建

Files in This Item:

There are no files associated with this item.


作者单位: Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing, China; Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Kunming, China

Recommended Citation:
Li M.-Y.,Wang L.,Fan Z.-X.,et al. Tree-ring density inferred late summer temperature variability over the past three centuries in the Gaoligong Mountains, southeastern Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015-01-01,422
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Li M.-Y.]'s Articles
[Wang L.]'s Articles
[Fan Z.-X.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Li M.-Y.]'s Articles
[Wang L.]'s Articles
[Fan Z.-X.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Li M.-Y.]‘s Articles
[Wang L.]‘s Articles
[Fan Z.-X.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.