“…Processes at the land-atmosphere interface are mainly driven by water and energy fluxes at the land surface, which are mediated by vegetation (Koch et al, 2017;Simon et al, 2021), land use, and topography. These surface fluxes have proved to control the overlying atmospheric distributions of water vapor, temperature, precipitation, and cloud properties, modulating the hydrological cycle and the surface energy budget (Dickinson, 1995;Dirmeyer et al, 2013;Y. Wang et al, 2023;Wu et al, 2015).…”