“…A good comprehension of the coupling which occurs at different spatial scales, from the plot to the watershed, between atmosphere, vegetation dynamics, and hydrological processes is important in different fields such as hydrometeorology, ecology, biogeochemical cycles, geochemistry of soil, and rock weathering. For example, a realistic representation of this coupling is necessary to address the following issues: the impacts of arid or semiarid climates on vegetation and soil erosion [ Rodriguez‐Iturbe et al ., ], the circulation of chemical nutrients in the soil (C, N, …) and the weathering of soil and rock minerals [ Zhang et al ., ; Goddéris et al ., ], the impacts of the climate change on vegetation or water resources, from the local to the regional scale [ Krinner et al ., ; Xia and Shao , ], the measures to propose to stakeholders for forest and water management [ Chen et al ., ]. Therefore, a hydrological model that incorporates vegetation and land surface processes is needed to accurately model at the different scales of interest the interactions and the feedbacks between atmospheric, vegetation, and water dynamics along the vertical soil‐vegetation‐atmosphere continuum and over time.…”