“…In this context, CPRCM forcing provides a major improvement for hydrological applications by providing further dynamical downscaling of several variables that require a fine spatio‐temporal resolution and in which the physical consistency between variables is preserved. Several studies have already used CPRCMs in hydrological applications to assess future flood risks in the United States (Dougherty & Rasmussen, 2020, 2021; Lackmann, 2013), Eastern Alps (Reszler et al, 2018), Texas (Wang & Wang, 2019; Zhang, Wang, & Wang, 2020), Colorado River basin (Mendoza et al, 2016), Ouagadougou (Senior et al, 2021), and in the UK (Kay et al, 2015; Rudd et al, 2020). CPRCMs have also been applied to estimate the water budget of East Africa (Finney et al, 2019), Himalayan basins (Li, Gochis, et al, 2017), California (Dougherty et al, 2020), but also for droughts and low flows analysis (Lee, Bae, & Im, 2019; Qing et al, 2020).…”