With the continuous warming of the global climate, the ecological environment and water resources in the Yangtze River Basin are apt to be affected. The analysis and study of the future precipitation change trend in the region will help to provide a theoretical basis for water resources management and ecological protection in the Yangtze River Basin. Based on the observed precipitation data and precipitation data output from 13 global climate models of the Sixth International Coupled Model Comparison Program (CMIP6) with bias correction, this paper evaluates the precipitation simulation ability of climate models in the Yangtze River Basin from 1995 to 2014. The temporal and spatial variation trends of precipitation in 2021-2040 (near term), 2041-2070 (middle term), and 2071-2100 (long term) are analyzed under four SSP scenarios (SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5). The results show that: ① The model data with bias correction can simulate the characteristics of precipitation well in the Yangtze River Basin on the spatial and temporal scale, which is close to the observed values. ② The annual precipitation in the Yangtze River Basin will increase significantly with the increase in the radiation forcing level. Compared with the historical period (1995-2014), the annual precipitation growth in each scenario is relatively flat in the near term, and the precipitation growth is the largest in the long term. In general, seasonal precipitation shows the largest increase in winter, and the increase in spring and summer precipitation is relatively gentle. In autumn, except for the negative value of the precipitation change rate in the near term under the scenario SSP3-7.0, the other scenarios and periods are slowly increasing with lower change rates. ③ Spatially, the regions with larger annual precipitation increase are concentrated on the source region of the Yangtze River and the middle and upper reaches of the Yangtze River with relatively less precipitation. The high value center of spring precipitation increase is in the source area and the north of the middle and upper reaches, while the precipitation change rate is low in the south of the basin. The precipitation increment in summer and autumn is relatively low, and the near term and middle-term precipitation in the northern part of the middle and upper reaches is lower than that in the historical period. In winter, the precipitation in the whole basin has increased, which shows that the precipitation change rate in the north of the Yangtze River Basin is the largest, and it is smaller in the south. [ABSTRACT FROM AUTHOR]