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A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE
Huang, R (Huang, Ru)1,2; Zhu, HF (Zhu, Haifeng)1,3; Liang, EY (Liang, Eryuan)1,3; Liu, B (Liu, Bo)4; Shi, JF (Shi, Jiangfeng)5; Zhang, RB (Zhang, Ruibo)6; Yuan, YJ (Yuan, Yujiang)6; Griessinger, J (Griessinger, Jussi)7
Source PublicationCLIMATE DYNAMICS
2019
Volume53Issue:5-6Pages:3221-3233
DOI10.1007/s00382-019-04695-3
Abstract

Climatic change is exhibiting significant effects on the ecosystem of the Tibetan Plateau (TP), a climate-sensitive area. In particularly, winter frost, freezing events and snow avalanche frequently causing severe effects on ecosystem and social economy, however, few long-term winter temperature records or reconstructions hinder a better understanding on variations in winter temperature in the vast area of the TP. In this paper, we present a minimum winter (November-February) temperature reconstruction for the past 668 years based on a tree-ring network (12 new tree-ring chronologies) on the southeastern TP. The reconstruction exhibits decadal to inter-decadal temperature variability, with cold periods occurring in 1423-1508, 1592-1651, 1729-1768, 1798-1847, 1892-1927, and 1958-1981, and warm periods in 1340-1422, 1509-1570, 1652-1728, 1769-1797, 1848-1891, 1928-1957, and 1982-2007. As suggested by the comparisons with existing winter temperature series and spatial correlations with Climatic Research Unit gridded data, our reconstruction is reliable and indicative, and it can represent large-scale winter temperature variability on the southeastern TP. Furthermore, it shows an overall agreement with winter temperature from the northeastern TP on decadal to inter-decadal timescales. It also shows the possible effects of volcanic eruption and reducing solar activity on the winter temperature variability for the past six centuries on the southeastern TP.

Subject AreaEnvironmental Sciences
WOS IDWOS:000483626900043
Language英语
Indexed BySCI
KeywordLast 400 Years Qilian Juniper Yangtze-river 2 Centuries Variability China Growth Chronologies Eruption Mountain
WOS Research AreaMeteorology & Atmospheric Sciences
WOS SubjectMeteorology & Atmospheric Sciences
Cooperation Status国际
ISSN0930-7575
Department环境变化与地表过程重点实验室
URL查看原文
PublisherSPRINGER
Citation statistics
Cited Times:12[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/9177
Collection图书馆
Corresponding AuthorZhu, HF (Zhu, Haifeng)
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Alpine Ecol, Beijing 100101, Peoples R China;
2.Univ Chinese Acad Sci, Beijing 10049, Peoples R China;
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;
4.Northwest Univ, Coll Urban & Environm Sci, Xian 710127, Shaanxi, Peoples R China;
5.Nanjing Univ, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China;
6.China Meteorol Adm, Inst Desert & Meteorol, Urumqi 830002, Peoples R China;
7.Friedrich Alexander Univ Erlangen Nuremberg, Inst Geog, D-91058 Erlangen, Germany.
Recommended Citation
GB/T 7714
Huang, R ,Zhu, HF ,Liang, EY ,et al. A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE[J]. CLIMATE DYNAMICS,2019,53(5-6):3221-3233.
APA Huang, R .,Zhu, HF .,Liang, EY .,Liu, B .,Shi, JF .,...&Griessinger, J .(2019).A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE.CLIMATE DYNAMICS,53(5-6),3221-3233.
MLA Huang, R ,et al."A tree ring-based winter temperature reconstruction for the southeastern Tibetan Plateau since 1340 CE".CLIMATE DYNAMICS 53.5-6(2019):3221-3233.
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