Projection of the global monsoon (GM) system is essential for water resource management, food security, and policymaking. Here we investigate projected changes in global monsoon area (GMA) and global monsoon intensity (GMI) with specific global warming levels, using two datasets of large-ensemble simulations. Both datasets project quasi-linear increases in GMA and GMI with global warming. The GMI over Northern-Hemisphere continents is consistently enhanced, while the GMI over Southern-Hemisphere continents are dominated by opposite changes in the GMI over South America. In addition, both datasets show enhanced monsoon intensity over most parts of regional monsoon domains, except for the North American monsoon. The different changes of the North American monsoon are up on projected temperature differences between the equatorial eastern Pacific and the tropical Atlantic. Moisture budget shows that the thermodynamic component always makes a large positive contribution to the increase in monsoon precipitation, while evaporation has a smaller positive contribution, except for the East Asian monsoon. The contribution of the dynamic component shows large differences for different regional monsoons. Therefore, the different changes in regional monsoon precipitation are mainly caused by the dynamic component.