Remote sensing (RS)-based two-source models have been widely used to separate soil
evaporation (E) and vegetation transpiration (T) in ecosystems. Alternative model …

Reducing water losses in agriculture needs a solid understanding of when evaporation (E)
losses occur and how much water is used through crop transpiration (T). Partitioning …

Catchment-scale efficient agricultural drought monitoring and irrigation planning mostly
depend on the accuracy of evapotranspiration (ET) estimates under different crop-growth …

Evapotranspiration (ET) is an important approach for enabling water and energy exchange
between the atmosphere and the land, and it has a very close relationship with terrestrial …

Identifying the unique change characteristics of evapotranspiration (ET) in the typical
vegetation of the semi-arid Loess Plateau and accurately estimating their components …

Land surface temperature-fractional vegetation coverage (LST-f c) trapezoid framework
based models have been widely developed, applied, and verified to estimate regional latent …

The stable water isotope method is widely applied to distinguish the evapotranspiration (ET)
components across various vegetation‐covered surfaces. ET partitioning in the urban …

A trapezoidal boundary location algorithm (TBLA) for the dry/wet boundaries of the land
surface temperature (T m)-fractional vegetation coverage (fc) trapezoidal framework is …

Estimation of urban evapotranspiration (ET) is meaningful for evaluating the urban heat
island effect and promoting urban water conservation. While multi-source satellite-based ET …

While evapotranspiration (ET) is normally measured as one hydrologic component,
evaporation (E), and transpiration (T) result from different physical‐biological processes …