Soil moisture (SM) is a key hydrologic state variable that is of significant importance for
numerous Earth and environmental science applications that directly impact the global …

▪ Abstract Soil moisture is spatially and temporally highly variable, and it influences a range
of environmental processes in a nonlinear manner. This leads to scale effects that need to …

Soil water content (SWC) plays a key role in partitioning water and energy fluxes at the land
surface and in controlling hydrologic fluxes such as groundwater recharge. Despite the …

The spatio-temporal dynamics of soil water content was investigated within a small
agricultural maize cropped field located in Belgium. Soil moisture measurements were …

Field hydrology is on the decline. Meanwhile, the need for new field‐derived insight into the
age, origin and pathway of water in the headwaters, where most runoff is generated, is more …

Soil moisture is a key variable in hydrology, meteorology and agriculture. It is influenced by
many factors, such as topography, soil properties, vegetation type, management, and …

Soil moisture refers to the water present in the uppermost part of a field soil and is a state
variable controlling a wide array of ecological, hydrological, geotechnical, and …

The use of surface soil water content data as additional input for the Root Zone Water
Quality Model in modeling profile soil water content was investigated at four field sites in the …

Characterization of soil hydraulic behavior at large scales using traditional methods is time-
consuming and very costly. Efficient and cheap means of providing hydrological models with …

The discipline of hydrology has long focused on quantifying the water balance, which is
frequently used to estimate unknown water fluxes or stores. While technologies for …