Soil hydrological processes (SHP) support ecosystems, modulate the impact of climate
change on terrestrial systems and control feedback mechanisms between water, energy and …

Groundwater is by far the largest unfrozen freshwater resource on the planet. It plays a
critical role as the bottom of the hydrologic cycle, redistributing water in the subsurface and …

Assessing root sources of three uncertainties–parameterization of soil hydraulic
characteristics, boundary conditions, and estimation of source/sink terms–is a significant …

Plant water stress occurs at the point when soil moisture (SM) limits transpiration, defining a
critical SM threshold (θcrit). Knowledge of the spatial distribution of θcrit is crucial for future …

The World Soil Information Service (WoSIS) provides quality-assessed and standardised
soil profile data to support digital soil map** and environmental applications at broadscale …

While large‐scale terrestrial evapotranspiration (ET) information is essential for our
understanding of the Earth's water and energy cycles, substantial differences exist in current …

Widespread adoption of improved cropland management measures is advocated to
increase soil organic carbon (SOC) levels, thereby improving soil fertility and mitigating …

Regional-scale hydrological investigations that involve vegetation change usually neglect
root-induced modification (RIM) of soil hydraulic properties (SHP). However, there is …

Water potential directly controls the function of leaves, roots and microbes, and gradients in
water potential drive water flows throughout the soil–plant–atmosphere continuum …

Accurate estimates of root zone soil moisture (RZSM) at relevant spatio-temporal scales are
essential for many agricultural and hydrological applications. Applications of machine …