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JOURNAL OF DESERT RESEARCH  2013, Vol. 33 Issue (5): 1536-1543    DOI: 10.7522/j.issn.1000-694X.2013.00220
Weather and Climate     
Change of Mean Maximum Temperature in July during 1506-2008 in Seda of West Sichuan Plateau According to Reconstructed Tree-ring Series
XIAO Ding-mu1, QIN Ning-sheng1,2,3, LI Jin-jian3, LI Yuan-yuan3
1.School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China;
2.Chengdu Institute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072;
3.The Agrometeorological Center of Sichuan Province, Chengdu 610072, China
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Abstract  

Tree-ring chronologies during 1506-2008 was constructed by tree-ring samples from Rejigou in West Sichuan Plateau. Correlation analysis indicated that the correlation were significant among tree-ring chronologies and mean maximum temperature in July at Seda meteorological station in West Sichuan Plateau, so a mean maximum temperature series in July during 1506-2008 at Seda was well reconstructed by the tree-ring chronology series and its explain variance was 39.7%. It was verified that the reconstructed series was reliable by leave-one-out cross-validation. The reconstructed series indicated there were five warm periods, which were 1512-1548, 1577-1590, 1612-1660, 1670-1687 and 1704-1784, and seven cold periods, which were 1549-1579, 1591-1611, 1688-1703, 1785-1828, 1837-1856, 1863-1902 and 1962-1998. Wavelet analysis showed that periods of the mean maximum temperature change in July were 80-130 years, 24-33 years, 7-16 years and 2-3 years.

Key words:  west Sichuan Plateau      tree-ring      climatic reconstruction      temperature change     
Received:  27 July 2012      Published:  28 August 2012
ZTFLH:  P467  

Cite this article: 

XIAO Ding-mu1, QIN Ning-sheng1,2,3, LI Jin-jian3, LI Yuan-yuan3. Change of Mean Maximum Temperature in July during 1506-2008 in Seda of West Sichuan Plateau According to Reconstructed Tree-ring Series. JOURNAL OF DESERT RESEARCH, 2013, 33(5): 1536-1543.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2013.00220     OR     http://www.desert.ac.cn/EN/Y2013/V33/I5/1536

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