“…The distributed hydrological model ESSI-3 was set up to capture the spatial-temporal variability of hydrological processes of the SJP. Briefly, The ESSI-3 model, which is based on energy balance and water balance and constituted with various basic modules (e.g., a remote sensing-based ET module, a three-layer soil water balance module, and a groundwater module) and specific hydrological process modules (e.g., permafrost hydrology, snow melting, and wetland hydrology), can accurately characterize various hydrological fluxes (e.g., runoff and ET) and states (e.g., SWE, CWS, SMS, and groundwater storage) (Zhang and Zhang, 2006;Liu et al, 2015;Chen and Zhang, 2019;Wang et al, 2022). Especially for this study, based on a remote sensing-based two-leaf Jarvis-type canopy conductance model (RST-Gc), the actual ET is partitioned into four parts, including wet canopy evaporation (E wet c ), saturated soil surface evaporation (E sat c ), wet soil evaporation (E moi c ), and dry canopy transpiration (E dry c ).…”