The Congnaisi region is located on the southern slope of the Central Tianshan Mountains in Xinjiang. Based on the tree-ring data analysis, mean maximum temperature from May to August of the Congnaisi region from 1777 to 2008 A.D. has been reconstructed by the tree-ring average gray values. The power spectrum analysis shows that there are 154-, 77-, 2.7- and 2.3-years cycles in the reconstruction, which may be associated with solar activity and quasi-biennial oscillation (QBO). The moving t-test indicates that the significant abrupt changes were presented in about 1842 A.D., 1880 A.D. and 1923 A.D.