The variation of monthly average soil temperature at 0. 8m, 1. 6m and 3. 2m deep layers in Kashi from 1981 to 2010 was investigated by using linear trend analysis and accumulated variance methods. The results showed that annual average soil temperature at deep layers of 0. 8m, 1. 6m and 3. 2m decreased from 1984 to 1992 significantly (P<0. 01) and increased significantly from 1996 to 2004 (P<0. 01), but the liner trend of soil temperature was not significant during the whole period. Soil temperature at different deep layers increases significantly in winter and spring but decreased significantly in summer and autumn, of which at 0. 8m layer in summer(P<0. 01), 1. 6m layer in autumn (P<0. 05) was significant respectively. From decadal variation, average soil temperature at different deep layer in 1980s was higher than that in 1990s and first 10 years of 21~(st)century. Air temperature variation was one of the main factors affecting deep layer soil temperature and there was positive correlation between them. Precipitation also had a certain impact on the deep soil temperature, and average soil deeper temperature was related to precipitation increasing. Annual average soil temperature at 0. 8m and 1. 6m depth had abrupt changes in 1985 and 2009, and 3. 2m depth was in 1985 and 2008 by the Mann-Kendall test. The results could provide scientific reference to adapt to climate change for Kashi.