Abstract: Using EOF,wavelet analysis and correlation method,distribution feature of spring rainfall and its relation to circulation anomaly are investigated.The results show that spring rainfall mainly concentrates in the center and eastern areas of the south to the North Latitude 30,but less in north.The spring rainfall increases in the west and decreases in the center and eastern areas,but not apparent.EOF1 shows that relation between rainfall to the south of Chang Jiang River and to north of Chang Jiang River is contrary.There are 2year,7year and 15year characteristic timescale for variability of a wide range rainfall to the south of Chang Jiang River,and 5year characteristic timescale has a tendency to move towards larger timescale.EOF2 shows that the distributions of rainfall in the South of China and the middle and lower Chang Jiang River are contrary.There are 2year,9year and lager characteristic timescale for variability of a wide range rainfall in middle and lower Chang Jiang River,and 9year characteristic timescale has a tendency to move towards smaller timescale.It is helpful for a wide range rainfall to the south of Chang Jiang River when subtropical high in the middle of Pacific ocean is increasing and extending to west while pressure-gradient force is increasing in north of subtropical high.It is helpful for a wide range rainfall in middle and lower Chang Jiang River when the subtropical high is moving to the north,extending to middle and lower Chang Jiang River and Ural Mountains blocking high is increasing.