Computing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) requires internal calibration of sensible heat flux using anchor pixels (“hot” and “cold” pixels). Despite the development of automated anchor pixel selection methods that classify a pool of candidate pixels using the amount of vegetation (normalized difference vegetation index, NDVI) and surface temperature (Ts), final pixel selection still relies heavily on operator experience. Yet, differences in final ET estimates resulting from subjectivity in selecting the final “hot” and “cold” pixel pair (from within the candidate pixe...
Due to the limited availability of land surface temperature (LST) images, thermal-based evapotranspi...
Accurate spatially distributed estimates of actual evapotranspiration (ET) derived from remotely sen...
The thesis emphasizes the pivotal role that the Monin-Obukhov length (L) can play within the energy ...
Computing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping...
ABSTRACT: A remaining challenge to applying satellite-based energy-balance algorithms for operationa...
Accurately estimating evapotranspiration (ET) at large spatial scales is essential to our understand...
The purpose of this research was to develop an automated calibration algorithm for the Mapping Evapo...
Mapping EvapoTranspiration at high Resolution using Internal Calibration (METRIC) is most widely use...
In typical surface energy balance (SEB) models such as surface energy balance for land (SEBAL) and m...
Evapotranspiration (ET) represents one of the key components of the terrestrial hydrological cycle. ...
ABSTRACT Surface temperature (Ts) is a determining factor to obtain energy balance parameters, being...
Accurately estimating evapotranspiration (ET) at large spatial scales is essential to our understand...
ABSTRACT: Agricultural irrigation accounts for a large fraction of the total water use in the wester...
Due to their image-based nature, “contextual” approaches are very attractive to estimate evapotransp...
Due to their image-based nature, "contextual" approaches are very attractive to estimate evapotransp...
Due to the limited availability of land surface temperature (LST) images, thermal-based evapotranspi...
Accurate spatially distributed estimates of actual evapotranspiration (ET) derived from remotely sen...
The thesis emphasizes the pivotal role that the Monin-Obukhov length (L) can play within the energy ...
Computing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping...
ABSTRACT: A remaining challenge to applying satellite-based energy-balance algorithms for operationa...
Accurately estimating evapotranspiration (ET) at large spatial scales is essential to our understand...
The purpose of this research was to develop an automated calibration algorithm for the Mapping Evapo...
Mapping EvapoTranspiration at high Resolution using Internal Calibration (METRIC) is most widely use...
In typical surface energy balance (SEB) models such as surface energy balance for land (SEBAL) and m...
Evapotranspiration (ET) represents one of the key components of the terrestrial hydrological cycle. ...
ABSTRACT Surface temperature (Ts) is a determining factor to obtain energy balance parameters, being...
Accurately estimating evapotranspiration (ET) at large spatial scales is essential to our understand...
ABSTRACT: Agricultural irrigation accounts for a large fraction of the total water use in the wester...
Due to their image-based nature, “contextual” approaches are very attractive to estimate evapotransp...
Due to their image-based nature, "contextual" approaches are very attractive to estimate evapotransp...
Due to the limited availability of land surface temperature (LST) images, thermal-based evapotranspi...
Accurate spatially distributed estimates of actual evapotranspiration (ET) derived from remotely sen...
The thesis emphasizes the pivotal role that the Monin-Obukhov length (L) can play within the energy ...