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A 2000-year temperature reconstruction in the Animaqin Mountains of the Tibet Plateau, China
Chen, F (Chen, Feng)1,2; Zhang, Y (Zhang, Yong)1,3; Shao, XM (Shao, Xuemei)1,3; Li, MQ (Li, MingQi)1; Yin, ZY (Yin, Zhi-Yong)1,4; Zhang, Y
Source PublicationHOLOCENE
2016
Volume26Issue:12Pages:1904-1913
DOI10.1177/0959683616646187
AbstractA 2665-year ring-width chronology was developed based on Qilian juniper from the upper treeline of the Animaqin Mountains on the eastern Tibetan Plateau. Correlation analysis results showed that the chronology was significantly negatively correlated with April-June maximum temperature at nearby meteorological stations, indicating that maximum temperature is the factor that limits tree growth in this area. Accordingly, we reconstructed the average April-June maximum temperature variations since 261 BC. Our regression model explained 37.9% of the total variance for the whole calibration period of 1960-2012. Our reconstruction revealed that the maximum temperature started to increase from approximately 1750 without a rapid warming trend, and the warmest period was from AD 890 to 947, as opposed to the recent period, whereas the period from AD 351-483 was the coldest. Significant periods in the wavelet power spectrum were approximately 2-8 years, 20-30 years, 30-60 years, and 60-130 years, as well as some long-term periods (more than 200 years). Comparisons with other temperature series from neighboring regions and the Northern Hemisphere as a whole support the validity of our reconstruction and suggest that it provides a representation of the temperature change for the Animaqin area, although asymmetric variation patterns in minimum and maximum temperatures were found.
Subject Area自然地理学
WOS IDWOS:000386909700002
Language英语
Indexed BySCI
KeywordTree-ring Record Northern-hemisphere Minimum Temperature Qinghai Province Last Millennium Qilian Juniper Climate-change Variability Maximum Oscillation
Cooperation Status国际
SubtypeArticle
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Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7491
Collection图书馆
Corresponding AuthorZhang, Y
Affiliation1.Chinese Acad Sci, Inst Geog Sci & Nat Resources, Key Lab Land Surface Pattern & Simulat, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Chinese Acad Sci, Ctr Excellence & Innovat Tibetan Plateau Earth Sy, Beijing, Peoples R China
4.Univ San Diego, Dept Environm & Ocean Sci, San Diego, CA 92110 USA
Recommended Citation
GB/T 7714
Chen, F ,Zhang, Y ,Shao, XM ,et al. A 2000-year temperature reconstruction in the Animaqin Mountains of the Tibet Plateau, China[J]. HOLOCENE,2016,26(12):1904-1913.
APA Chen, F ,Zhang, Y ,Shao, XM ,Li, MQ ,Yin, ZY ,&Zhang, Y.(2016).A 2000-year temperature reconstruction in the Animaqin Mountains of the Tibet Plateau, China.HOLOCENE,26(12),1904-1913.
MLA Chen, F ,et al."A 2000-year temperature reconstruction in the Animaqin Mountains of the Tibet Plateau, China".HOLOCENE 26.12(2016):1904-1913.
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