Water storage capacity of forest ecosystems related to water regulation services (WSCFE) refers to the redistribution, reuse, and recycling of precipitation through three vertical layers: canopy (Aydin et al., 2018), litter (Zagyvai-Kiss et al., 2019), and soil (Olarieta et al., 2017). Water regulation, which is related to the hydrological cycle, water flow maintenance, and flood protection, is one of the important ecosystem services (Ouyang et al., 2016). Specifically, the water regulation function includes maintaining humidity in the canopy layer, avoiding direct erosion of soil by precipitation in the litter layer, and regulating flood, runoff and water storage in the soil layer. For example, the North American forest-covered regions (Duan et al., 2016;Hallema et al., 2018) and South American rainforests (Jones et al., 2017) generate and recycle over 50% of water consumed to maintain ecosystem function and integrity, and part of this water is used for evapotranspiration. Although several studies have considered water flux based on water balance (Milly, 1994;Willmott et al., 1985), the spatial pattern of WSCFE and the factors controlling WSCFE have not been fully investigated at the global scale.Due to the high monetary and labor costs required for long-term observations as well as the absence of open observed data (Rodell et al., 2018), WSCFE is difficult to assess using field measurements on a global scale. Some ecosystem service models such as the Integrated Valuation of Ecosystem Services and Trade-offs and Artificial Intelligence for Ecosystem Services models can be used to simulate WSCFE globally; however, the simulation results have not typically been validated on a large scale with observation data. The Gravity Recovery and Climate Experiment (GRACE) mission tracked groundwater depletion, reservoir changes, surface water, and