A number of energy balance models of variable complexity that use remotely sensed boundary conditions for producing spatially distributed maps of surface fluxes have been proposed. Validation typically involves comparing model output to flux tower observations at a handful of sites, and hence there is no way of evaluating the reliability of model output for the remaining pixels comprising a scene. To assess the uncertainty in flux estimation over a remote sensing scene requires one to conduct pixel-by-pixel comparisons of the output. The objective of this paper is to assess whether the simplifications made in a simple model lead to erroneous predictions or deviations from a more complex model and under which circumstances these deviations m...
A correct estimation of both the temporal and spatial distribution of evapotranspiration (ET) is ess...
Accurate estimation of spatial distributions of water (evapotranspiration) and energy fluxes is a go...
The two-source energy balance (TSEB) model uses remotely sensed maps of land–surface temperature (LS...
A number of energy balance models of variable complexity that use remotely sensed boundary condition...
A number of energy balance models of variable complexity that use remotely sensed boundary condition...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
Reliable estimation of the surface energy balance from local to regional scales is crucial for many ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
A correct estimation of both the temporal and spatial distribution of evapotranspiration (ET) is ess...
Accurate estimation of spatial distributions of water (evapotranspiration) and energy fluxes is a go...
The two-source energy balance (TSEB) model uses remotely sensed maps of land–surface temperature (LS...
A number of energy balance models of variable complexity that use remotely sensed boundary condition...
A number of energy balance models of variable complexity that use remotely sensed boundary condition...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
In most hydrologic modeling studies, the hypothesis is made that an improvement in the modeled soil ...
Reliable estimation of the surface energy balance from local to regional scales is crucial for many ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
A correct estimation of both the temporal and spatial distribution of evapotranspiration (ET) is ess...
Accurate estimation of spatial distributions of water (evapotranspiration) and energy fluxes is a go...
The two-source energy balance (TSEB) model uses remotely sensed maps of land–surface temperature (LS...