Changes in global and regional precipitation characteristics are among the most relevant aspects of climate change in a warming world (IPCC, 2021). Climate models are valuable tools for studying climate variability and climate change; however, the current state-of-the-art climate models generally show significant biases in simulating precipitation, especially its extremes (Grose et al., 2020;Kao & Ganguly, 2011;Toreti et al., 2013). Climate models represent small-scale processes such as convection using sub-grid models known as parameterizations, and these parameterizations contribute substantially to uncertainty in precipitation projections (Bony et al., 2015;Daleu et al., 2016;Wilcox and Donner, 2007). Precipitation characteristics are also greatly dependent on topography, orography, and spatial variations, which the coarse resolution of climate models fail to represent accurately.There are broadly two reasons why a finer grid might improve an atmospheric or climate simulation. First, better numerical resolution of processes such as atmospheric convection, eddies or land-atmosphere interactions and topographic effects could produce more accurate calculations on all scales, even to global-scale circulations or phenomena like El Nino. Second, for a given large-scale accuracy, a more refined grid could add local detail that a coarser grid cannot resolve. How valuable this detail will depend on the situation; for initial-value numerical weather prediction, for example, any detail that observations can constrain is important, and forecast centers run at the highest affordable resolutions (now approaching 10 km for global domains). For climate applications, the benefits are harder to verify and may derive mainly from detail in the boundary conditions (land surface and orography).From an ensemble of regional and global climate simulations (RCM and GCM, respectively), previous studies have concluded that precipitation intensity increases with increases in spatial resolution (Bador et al., 2020;