Understanding the contributions of soil water evaporation (E) and crop transpiration (T) to
evapotranspiration (ET) is essential for irrigation management and improving crop water use …

The cylindrical-perfect-conductors (CPC) theory, which assumes an infinite and
homogeneous soil medium, can be used to analyze heat pulse (HP) measurements to …

Unsaturated hydraulic conductivity (K) of surface soil changes substantially with space and
time, and it is of great importance for many ecological, agricultural, and hydrological …

Soil ice content is an important component for winter soil hydrology. The sensible heat
balance (SHB) method using measurements from heat pulse probes (HPPs) is a possible …

Soil heat flux at the surface (G 0) is strongly influenced by whether the soil is shaded or
sunlit, and therefore can have large spatial variability for incomplete vegetation cover, such …

The Integrated Carbon Observation System is a pan-European research infrastructure
providing standardized, long-term observations of greenhouse gas concentrations and …

Soil‐surface heat flux (G 0), an important component of the surface energy balance, is often
determined by summing soil heat flux (Gz) at a depth (z) below the surface and the rate of …

A thermo‐time domain reflectometry (thermo‐TDR) sensor combines a heat‐pulse sensor
with a TDR waveguide to simultaneously measure coupled processes of water, heat, and …