Evapotranspiration partitioning at the ecosystem scale using the stable isotope method—A review
Terrestrial evapotranspiration (ET) consists of evaporation (E) from canopy-intercepted
water, evaporation from soil and open water, and transpiration (T) from plants. Determining …
water, evaporation from soil and open water, and transpiration (T) from plants. Determining …
Ecosystem transpiration and evaporation: Insights from three water flux partitioning methods across FLUXNET sites
We apply and compare three widely applicable methods for estimating ecosystem
transpiration (T) from eddy covariance (EC) data across 251 FLUXNET sites globally. All …
transpiration (T) from eddy covariance (EC) data across 251 FLUXNET sites globally. All …
Reviews and syntheses: Turning the challenges of partitioning ecosystem evaporation and transpiration into opportunities
Evaporation (E) and transpiration (T) respond differently to ongoing changes in climate,
atmospheric composition, and land use. It is difficult to partition ecosystem-scale …
atmospheric composition, and land use. It is difficult to partition ecosystem-scale …
A simple and objective method to partition evapotranspiration into transpiration and evaporation at eddy-covariance sites
Separating evapotranspiration (ET) into evaporation (E) and transpiration (T) is challenging
but key for a better understanding and prediction of the hydrological cycle and plant water …
but key for a better understanding and prediction of the hydrological cycle and plant water …
Recent increase in the observation-derived land evapotranspiration due to global warming
Estimates of change in global land evapotranspiration (ET) are necessary for understanding
the terrestrial hydrological cycle under changing environments. However, large uncertainties …
the terrestrial hydrological cycle under changing environments. However, large uncertainties …
An increasing trend in the ratio of transpiration to total terrestrial evapotranspiration in China from 1982 to 2015 caused by greening and warming
The ratio of transpiration to total terrestrial evapotranspiration (T/ET) plays an important role
in the hydrological cycle and in the energy budgets between the land and the atmosphere …
in the hydrological cycle and in the energy budgets between the land and the atmosphere …
Water availability impacts on evapotranspiration partitioning
Knowing how evapotranspiration (ET) is mediated by abiotic and biotic pathways is
essential to understanding how water affects ecosystem productivity. Recent studies have …
essential to understanding how water affects ecosystem productivity. Recent studies have …
Sun-induced fluorescence closely linked to ecosystem transpiration as evidenced by satellite data and radiative transfer models
Transpiration (T) returns about half of continental precipitation back into the atmosphere.
However, the global spatial and temporal dynamics of transpiration are highly uncertain, and …
However, the global spatial and temporal dynamics of transpiration are highly uncertain, and …
Hydroclimatic response of evapotranspiration partitioning to prolonged droughts in semiarid grassland
A warming climate is expected to perturb the hydrological cycle, resulting in changes to both
the frequency and duration of drought, especially in arid and semiarid grassland. Although …
the frequency and duration of drought, especially in arid and semiarid grassland. Although …
Coupling water and carbon fluxes to constrain estimates of transpiration: The TEA algorithm
Plant transpiration (T), biologically controlled movement of water from soil to atmosphere,
currently lacks sufficient estimates in space and time to characterize global ecohydrology …
currently lacks sufficient estimates in space and time to characterize global ecohydrology …