Sensible and latent heat fluxes are often calculated from bulk transfer equations combined with the energy balance. For spatial estimates of these fluxes, a combination of remotely sensed and standard meteorological data from weather stations is used. The success of this approach depends on the accuracy of the input data and on the accuracy of two variables in particular: aerodynamic and surface conductance. This paper presents a Bayesian approach to improve estimates of sensible and latent heat fluxes by using a priori estimates of aerodynamic and surface conductance alongside remote measurements of surface temperature. The method is validated for time series of half-hourly measurements in a fully grown maize field, a vineyard and a forest...
A method to estimate the sensible heat flux (H) for unstable atmospheric condition requiring measure...
In this paper we pledge that physically based equations should be combined with remote sensing techn...
A scheme is proposed that relates surface flux densities of sensible heat, latent heat, and momentum...
Sensible and latent heat fluxes are often calculated from bulk transfer equations combined with the ...
The influence of uncertainty in land surface temperature, air temperature, and wind speed on the est...
An approach to the remote sensing of land surface temperature is developed using the methods of Baye...
The approach of using remote sensing of surface temperature to estimate spatially distributed surfac...
Surface heat fluxes (latent and sensible heat over the land surface) play a key role in the land-atm...
In this paper, the relationships between NDVI (normalized difference vegetation index) and pseudo th...
Equations based on surface renewal (SR) analysis to estimate the sensible heat flux (H) require as i...
A surface energy balance was conducted to calculate the latent heat flux (λE) using aerodynamic meth...
A series of energy-balance experiments were performed over a winter wheat field in Southern Arizona....
The partitioning of available energy between sensible heat and latent heat is important for precise ...
A simple two-source evapotranspiration (ET) model was applied to the Yingke and Daman irrigation dis...
The overall topic of the research described 10 this dissertation was the partitioning of available e...
A method to estimate the sensible heat flux (H) for unstable atmospheric condition requiring measure...
In this paper we pledge that physically based equations should be combined with remote sensing techn...
A scheme is proposed that relates surface flux densities of sensible heat, latent heat, and momentum...
Sensible and latent heat fluxes are often calculated from bulk transfer equations combined with the ...
The influence of uncertainty in land surface temperature, air temperature, and wind speed on the est...
An approach to the remote sensing of land surface temperature is developed using the methods of Baye...
The approach of using remote sensing of surface temperature to estimate spatially distributed surfac...
Surface heat fluxes (latent and sensible heat over the land surface) play a key role in the land-atm...
In this paper, the relationships between NDVI (normalized difference vegetation index) and pseudo th...
Equations based on surface renewal (SR) analysis to estimate the sensible heat flux (H) require as i...
A surface energy balance was conducted to calculate the latent heat flux (λE) using aerodynamic meth...
A series of energy-balance experiments were performed over a winter wheat field in Southern Arizona....
The partitioning of available energy between sensible heat and latent heat is important for precise ...
A simple two-source evapotranspiration (ET) model was applied to the Yingke and Daman irrigation dis...
The overall topic of the research described 10 this dissertation was the partitioning of available e...
A method to estimate the sensible heat flux (H) for unstable atmospheric condition requiring measure...
In this paper we pledge that physically based equations should be combined with remote sensing techn...
A scheme is proposed that relates surface flux densities of sensible heat, latent heat, and momentum...