In recent years, the serious consequences of global warming have become a greater concern for the wide international community. The existing research into the eastern China monsoon region has discussed either an area or the whole region and had different emphases. Recently there have been few studies about the periods and abrupt features of different regional climate change in the eastern monsoon region. Base on the linear trend analysis, Mann- Kendall mutation test and Morlet wavelet, the regional annual average temperature and annual precipitation were analysed by using 20 sites monthly temperature and precipitation data from 1960-2012 in eastern China monsoon region. The results show that the whole region is getting warmer. Abrupt climate changes occurred in 1990s and the northeast underwent earlier changes than other areas. The increasing of temperature in the northern area was higher than the southern area. There existed an about-4-year cycle and a 8~12 year quasi-period. High frequency periodic variations of temperature were more obvious in the inland areas. The precipitation in the Sichuan Basin, Northern China and northwest of the monsoon region decreased. Precipitation in the lower part of the Changjiang river basin showed an increasing trend and other areas did not change significantly. There existed a 2~4 year cycle, and an 8~16 year quasi-period and the low frequency periodic variations of precipitation were more obvious in the offshore areas.