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Early-summer temperature variations over the past 563 yr inferred from tree rings in the Shaluli Mountains, southeastern Tibet Plateau

Published online by Cambridge University Press:  20 January 2017

Yang Deng ,
Xiaohua Gou ,
Linlin Gao ,
Tao Yang  and
Meixue Yang
Yang Deng
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change, Lanzhou University, Lanzhou 73000, China
Xiaohua Gou*
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change, Lanzhou University, Lanzhou 73000, China
Linlin Gao
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change, Lanzhou University, Lanzhou 73000, China
Tao Yang
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change, Lanzhou University, Lanzhou 73000, China
Meixue Yang
Affiliation:
State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
*
*Corresponding author. E-mail address:xhgou@lzu.edu.cn (X. Gou).
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Abstract

We developed a tree-ring chronology (AD 1446–2008) based on 75 cores from 37 Abies squamata Mast. trees from the Shaluli Mountains, southeastern Tibet Plateau, China, using signal-free methods, which are ideally suited to remove or reduce the distortion introduced during traditional standardization. This chronology correlates best with regional temperatures in June–July, which allowed us to develop a June–July temperature reconstruction that explained 51.2% of the variance in the instrumental record. The reconstruction showed seven cold periods and five warm periods. Cold periods were identified from AD 1472 to 1524, 1599 to 1653, 1661 to 1715, 1732 to 1828, 1837 to 1847, 1865 to 1876 and 1907 to 1926. Warm intervals occurred from AD 1446 to 1471, 1525 to 1598, 1716 to 1731, 1848 to 1864, 1877 to 1906 and 1927 to present. The reconstruction agrees well with nearby tree-ring-based temperature reconstructions. Spatial correlation analyses suggest that our reconstructions provide information on June–July temperature variability for the southeastern Tibetan Plateau and its vicinity. Spectral analyses revealed significant peaks at 2–6, 10.7, 51.2, 102.2 and 204.8 yr. The temperature variability in this area may be affected by ENSO, the Pacific Decadal Oscillation and solar activity.

Keywords

Tree ringsTemperature reconstructionClimate variabilitySoutheastern Tibet Plateau
Type
Articles
Information
Quaternary Research , Volume 81 , Issue 3 , May 2014 , pp. 513 - 519
Copyright
University of Washington

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References

Braun, H., Christl, M., Rahmstorf, S., Ganopolski, A., Mangini, A., Kubatzki, C., Roth, K., and Kromer, B. Possible solar origin of the 1,470-year glacial climate cycle demonstrated in a coupled model. Nature 438, (2005). 208–211.CrossRefGoogle Scholar
Cohen, J.L., Furtado, J.C., Barlow, M., Alexeev, V.A., and Cherry, J.E. Asymmetric seasonal temperature trends. Geophysical Research Letters 39, (2012). L04705 CrossRefGoogle Scholar
Cook, E.R., and Kairiukstis, L.A. Methods of Dendrochronology. (1990). Kluwer Dordrecht, CrossRefGoogle Scholar
D'Arrigo, R., Wilson, R., and Jacoby, G. On the long-term context for late twentieth century warming. Journal of Geophysical Research D: Atmospheres 111, (2006). D03103 CrossRefGoogle Scholar
D'Arrigo, R., Wilson, R., Liepert, B., and Cherubini, P. On the ‘Divergence Problem’ in Northern Forests: a review of the tree-ring evidence and possible causes. Global and Planetary Change 60, (2008). 289–305.CrossRefGoogle Scholar
Decker, K.L.M., Wang, D., Waite, C., and Scherbatskoy, T. Snow removal and ambient air temperature effects on forest soil temperatures in northern Vermont. Soil Science Society of America Journal 67, (2003). 1234–1242.CrossRefGoogle Scholar
Ding, Y., and Chan, J.C.L. The East Asian summer monsoon: an overview. Meteorology and Atmospheric Physics 89, (2005). 117–142.Google Scholar
Domrös, M., and Peng, G. The Climate of China. (1988). Springer-Verlag, CrossRefGoogle Scholar
Duan, J., Wang, L., Li, L., and Chen, K. Temperature variability since A.D. 1837 inferred from tree-ring maximum density of Abies fabri on Gongga Mountain, China. Chinese Science Bulletin 55, (2010). 3015–3022.CrossRefGoogle Scholar
Fan, Z., Bräuning, A., Tian, Q., Yang, B., and Cao, K. Tree ring recorded May–August temperature variations since A.D. 1585 in the Gaoligong Mountains, southeastern Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology 296, (2010). 94–102.CrossRefGoogle Scholar
Fang, K.Y., Gou, X.H., Chen, F.H., Li, J.B., D'Arrigo, R., Cook, E., Yang, T., and Davi, N. Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability. Climate Dynamics 35, (2010). 577–585.CrossRefGoogle Scholar
Gao, L., Gou, X., Deng, Y., Liu, W., Yang, M., and Zhao, Z. Climate–growth analysis of Qilian juniper across an altitudinal gradient in the central Qilian Mountains, northwest China. Trees - Structure and Function 27, (2013). 379–388.CrossRefGoogle Scholar
Gou, X., Chen, F., Yang, M., Gordon, J., Fang, K., Tian, Q., and Zhang, Y. Asymmetric variability between maximum and minimum temperatures in Northeastern Tibetan Plateau: evidence from tree rings. Science in China Series D: Earth Sciences 51, (2008). 41–55.CrossRefGoogle Scholar
Holmes, R.L. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 43, (1983). 69–78.Google Scholar
IPCC, Climate Change 2007: The Physical Science Basis: Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. (2007). Elsevier Inc., Google Scholar
Kamenos, N.A. North Atlantic summers have warmed more than winters since 1353, and the response of marine zooplankton. Proceedings of the National Academy of Sciences 107, (2010). 22442–22447.CrossRefGoogle ScholarPubMed
Kumar, K.K., Rajagopalan, B., and Cane, M.A. On the weakening relationship between the Indian monsoon and ENSO. Science 284, (1999). 2156–2159.CrossRefGoogle ScholarPubMed
Li, Z., Liu, G., Zhang, Q., Hu, C., Luo, S., Liu, X., and He, F. Tree ring reconstruction of summer temperature variations over the past 159 years in Wolong National Natural Reserve, western Sichuan, China. Chinese Journal of Plant Ecology 34, (2010). 628–641. (In Chinese with English Abstract) Google Scholar
Li, Z., Liu, G., Fu, B., Zhang, Q., Hu, C., and Luo, S. Tree-ring based summer temperature reconstruction over the past 200 years in Miyaluo of western Sichuan, China. Quaternary Sciences 31, (2011). 522–534. (In Chinese with English Abstract) Google Scholar
Li, Z., Zhang, Q., and Ma, K. Tree-ring reconstruction of summer temperature for A.D. 1475–2003 in the central Hengduan Mountains, Northwestern Yunnan, China. Climatic Change 110, (2012). 455–467.CrossRefGoogle Scholar
Liang, E.Y., Shao, X.M., and Qin, N.S. Tree-ring based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global and Planetary Change 61, (2008). 313–320.CrossRefGoogle Scholar
Mann, M.E., and Lees, J.M. Robust estimation of background noise and signal detection in climatic time series. Climatic Change 33, (1996). 409–445.CrossRefGoogle Scholar
Melvin, T.M., and Briffa, K.R. A “signal-free” approach to dendroclimatic standardisation. Dendrochronologia 26, (2008). 71–86.CrossRefGoogle Scholar
Minobe, S. A 50–70 year climatic oscillation over the North Pacific and North America. Geophysical Research Letters 24, (1997). 683–686.CrossRefGoogle Scholar
Mitchell, T.D., and Jones, P.D. An improved method of constructing a database of monthly climate observations and associated high-resolution grids. International Journal of Climatology 25, (2005). 693–712.CrossRefGoogle Scholar
Philander, S. El Niño southern oscillation phenomena. Nature 302, (1983). 295–301.CrossRefGoogle Scholar
Shao, X., and Fan, J. Past climate on west Sichuan plateau as reconstructed from ring-widths of dragon spruce. Quaternary Sciences 81–89, (1999). (In Chinese with English Abstract) Google Scholar
Song, H., Liu, Y., Ni, W., Cai, Q., Sun, J., Ge, W., and Xiao, W. Winter mean lowest temperature derived from tree-ring width in Jiuzhaigou region, China since 1750 A.D. Quaternary Science 27, (2007). 486–491. (In Chinese with English Abstract) Google Scholar
Wang, X., and Zhang, Q. Evidence of solar signals in tree rings of Smith fir from Sygera Mountain in southeast Tibet. Journal of Atmospheric and Solar-Terrestrial Physics 73, (2011). 1959–1966.CrossRefGoogle Scholar
Way, D.A., and Oren, R. Differential responses to changes in growth temperature between trees from different functional groups and biomes: a review and synthesis of data. Tree Physiology 30, (2010). 669–688.CrossRefGoogle ScholarPubMed
Wigley, T., Briffa, K.R., and Jones, P.D. On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. Journal of Applied Meteorology 23, (1984). 201–213.Google Scholar
Wilson, R., Cook, E., D'Arrigo, R., Riedwyl, N., Evans, M.N., Tudhope, A., and Allan, R. Reconstructing ENSO: the influence of method, proxy data, climate forcing and teleconnections. Journal of Quaternary Science 25, (2010). 62–78.CrossRefGoogle Scholar
Wu, P., Wang, L., and Shao, X. Reconstruction of summer temperature from maximum latewood density of Pinus densata in West Sichuan. Acta Geographica Sinica 60, (2005). 998–1006. (In Chinese with English Abstract) Google Scholar
Xu, H., Hong, Y.T., Hong, B., Zhu, Y.X., and Wang, Y. Influence of ENSO on multi-annual temperature variations at Hongyuan, NE Qinghai–Tibet plateau: evidence from δ13C of spruce tree rings. International Journal of Climatology 30, (2010). 120–126.CrossRefGoogle Scholar
Yu, S., Yuan, Y., Wei, W., Zhang, T., Shang, H., and Chen, F. Reconstructed mean temperature in Mearkang, West Sichuan in July and its detection of climatic period signal. Plateau Meteorology 31, (2012). 193–200. (In Chinese with English Abstract) Google Scholar
Zhu, H., Shao, X., Yin, Z., Xu, P., Xu, Y., and Tian, H. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings. Palaeogeography, Palaeoclimatology, Palaeoecology 305, (2011). 84–92.CrossRefGoogle Scholar