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Ring-widths of Abies at tree-line ecotone reveal three centuries of early winter season temperature changes in Yunnan, China

Authors :
Wei Huang
Yingfeng Bi
Xuefei Yang
Zhikun Wu
Jingchao Yang
Jianwen Li
Zenxin Fan
Whitney Cory
Source :
Climate Dynamics. 55:945-959
Publication Year :
2020
Publisher :
Springer Science and Business Media LLC, 2020.

Abstract

Variation in winter temperature is less well understood than in annual and summer temperatures over long timescales, particularly in low-latitude (0–30° N) montane regions with large spatial and topographic heterogeneity. Understanding these variations could be critical for forest manageemnt in these important tree growing regions. We collected tree-ring cores from Yunnan Province in montane southwest China, to determine how winter temperature has varied in the past and to explore its possible drivers in this region. Six highly correlated site chronologies were combined into a long and well-replicated regional composite (RC) chronology. The RC chronology correlated strongest with mean early winter season temperature (EWST) from November to January during 1959–2015. We applied RC chronology to reconstruct EWST from 1653 to 2015. The reconstruction shows five relatively warm historic intervals (1658–1718, 1743–1755, 1771–1791, 1929–1959, and 1995–2015) and cold intervals (1720–1742, 1792–1852, 1860–1883, 1905–1928, and 1960–1994). The 1950s with six anomalous warm seasons and 1980s with five anomalous cold seasons were the warmest and coldest decades, respectively. The EWST reconstruction generally agreed with other winter temperature reconstructions from nearby areas and with historical documents. Atlantic Multidecadal Oscillation (AMO) might be a key forcing of multidecadal winter temperature variations in montane southwest China over the past three and half centuries. Both warm and cold temperature periods coincide with respective positive and negative phases of AMO. Besides, the cold intervals during the nineteenth and twentieth centuries may also have been influenced by large volcano eruptions in low-latitude regions of south and east Asia. Our EWST reconstruction not only improves our understanding of the trends and variations of winter climate history, but also supports planning for resilience in conservation, agriculture, and forestry management in montane southwest China into the future.

Details

ISSN :
14320894 and 09307575
Volume :
55
Database :
OpenAIRE
Journal :
Climate Dynamics
Accession number :
edsair.doi...........8e7cc3a3e746c36564a9e0c5aa39cc81
Full Text :
https://doi.org/10.1007/s00382-020-05303-5