Water use efficiency (WUE) is a key index for understanding the ecosystem of carbon–water
coupling. The undistinguishable carbon–water coupling mechanism and uncertainties of …

Actual evapotranspiration (AET) is one of the decisive factors controlling the water balance
at the catchment level, particularly in arid and semi-arid regions, but measured data for …

Terrestrial evapotranspiration (ET) refers to a key process in the hydrological cycle by which
water is transferred from the Earth's surface to lower atmosphere. With spatiotemporal …

Evapotranspiration (ET) estimation models can be broadly classified as statistical or physical
process based models. However, assuming the limitation of individual approaches, the …

Understanding the long-term variation in evapotranspiration (ET) for the spatially distributed
grasslands is crucial for the accurate prediction of ET response to climate change. In this …

Urban flood-related issues are substantial in China, arising from rapid construction of
megacities over decades with insufficient flood control, all being made worse by climate …

Remote Sensing-based two-source model is widely used to estimate crop
evapotranspiration (ET), involving one key step of partitioning land surface temperature …

Remotely sensed land surface temperature (LST) is critical for retrieving evapotranspiration
(ET). However, due to cloud contamination, LST is often limited to clear-sky conditions and …

Urbanization substantially changes many aspects including the regional hydrological cycle,
energy balance, and microclimate. However, the degree to which urbanization alters urban …

Partition of land surface evapotranspiration (ET) into soil evaporation (ET soil) and
vegetation transpiration (ET veg) is of great significance for scheduling agricultural irrigation …