“…Many approaches are available to discretize the spatial derivatives in RRE (Bergamaschi & Putti, ; Farthing, Kees, & Miller, ), such as finite element method (Simunek et al, ), finite difference method (Dogan & Motz, ), finite volume method (Caviedes‐Voullième, Garcı´a‐Navarro, & Murillo, ; Svyatskiy & Lipnikov, ), finite analytical method (Zhang et al, ), etc. Under atmospheric boundary conditions (i.e., combinations of sinusoidal flux), the magnitudes of the hydraulic gradient, as well as vertical flux variations, generally dampen from the soil surface to deep soils (Bakker & Nieber, ; Dickinson et al, ).…”