Abstract: The western North Pacific tropical cyclone (TC) is one of the most significant weather systems affecting precipitation of China. The TC remnant low pressure systems (TCRL) still carry abundant moisture and energy, causing heavy rainfall along the TCRL's track. In order to analyze the impact of TCRL to precipitation of China, the objective methods were applied to identify TC cyclones based on the ERA-40 and ERA-Interim reanalysis, and thus obtain the TCRL tracks. The tracks of TCRL were classified to 3 categories, they were the Northeastward one (NE), Southeastern coast one (SEC) and Westward one (WW). TCRL effected precipitation distribution was obtained with the objective synoptic analysis technique (OSAT). Using this technique, we could track whole life history of TCs. There were 706 cyclones in total tracked from the 718 TCs that entered into the warning region during 1958-2014, and the average distance between the cyclone center and the TC center is 131 km. A total of 443 TCs had corresponding TCRLs which sustained for 48.5 hours on average, among which 293 TCRLs' lifetime lasted more than 1 day, to account for 66.1%. TCRLs' duration had no significant relationship with TCs' intensity. Lifetime of the TCRLs in summer was longer than that in winter. The influence to China inland of TCRLs was more obvious than TCs. TCRLs, whose influence range is larger than that of TC, brought more precipitation in southeastern China, and less precipitation in northwestern China. NE TCRLs entered the area of northeastern and eastern China, bringing precipitation mainly in eastern China. SEC TCRLs' influence was the widest, bringing the strongest precipitation. WW TCRLs entered only southern and southwestern China, bringing the weakest precipitation mainly in southern China.