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Temperature reconstruction from tree-ring maximum density of Balfour spruce in eastern Tibet, China
Wang L.; Duan J. P.; Chen J.; Huang L.; Shao X. M.
Source PublicationInternational Journal of Climatology
2010
Volume30
Issue7
Pages972-979
KeywordBalfour Spruce Maximum Latewood Density Temperature Reconstruction Wavelet Analysis Eastern Tibet Summer Temperature Northern Quebec Black Spruce Light Rings Climate Plateau Variability Conifers Europe Canada
AbstractWood from Balfour spruce [Picea likiangensis var. balfburiana (Rehd. et Wils.)] was collected at three sites in eastern Tibet. Maximum latewood densities (MXD) were measured by X-ray densitometry; individual series were first cross dated and then combined to form a standard chronology. This chronology was significantly correlated with late summer temperatures on the eastern Tibetan Plateau. It was used to reconstruct the August-September mean temperature for the period 1695-2000 A.D., and it explained the 63.5% of the total temperature variance. Wavelet analysis of the reconstructed temperature series suggested the existence of a 20-year climatic cycle during the period 1800-1860 and a similar to 50-year cycle at the beginning of the twentieth century. Copyright (C) 2009 Royal Meteorological Society
Indexed BySCI
Language英语
ISSN0899-8418
Document TypeSCI/SSCI论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/22905
Collection历年回溯文献
Recommended Citation
GB/T 7714
Wang L.,Duan J. P.,Chen J.,et al. Temperature reconstruction from tree-ring maximum density of Balfour spruce in eastern Tibet, China. 2010.
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