Monitoring of water and energy fluxes is a requirement for assessment of climate and anthropogenic effects on natural and agricultural ecosystems [i]. These fluxes consist of the physical transfers between soil, vegetation and atmosphere. In order to describe these transfers, on local, regional or global scale, and the changes taking place in the compartments it is necessary to have measurements and models to estimate these fluxes. Distributed hydrological models are appropriate tools and are constantly improving the understanding of this cycling of water through soils, vegetation and atmosphere. Also for the relatively new emerging field of ecohydrology estimation of spatially distributed water and energy levels is essential for predicting...
Terrestrial evapotranspiration (ET) is a central process in the climate system, is a major component...
Understanding the spatial variability in highly heterogeneous natural environments such as savannas ...
As the worlds water resources come under increasing tension due to dual stressors of climate change ...
Monitoring of water and energy fluxes is a requirement for assessment of climate and anthropogenic e...
A correct estimation of both the temporal and spatial distribution of evapotranspiration (ET) is ess...
This edition of Evapotranspiration - Remote Sensing and Modeling contains 23 chapters related to the...
Reliably and accurately quantifying evapotranspiration (ET) in a spatial and temporal domain is impo...
Studies of global hydrologic cycles, carbon cycles and climate change are greatly facilitated when. ...
Accurate estimation of spatial distributions of water (evapotranspiration) and energy fluxes is a go...
The mountains are known as the water towers of the World and they are also climate hot spots. Theref...
Thermal-infrared remote sensing of land surface temperature provides valuable information for quanti...
In semiarid areas, agricultural production is restricted by water availability; hence, efficient agr...
Being a major component of the hydrological cycle, evapotranspiration (ET) and its spatial and tempo...
Evapotranspiration (ET) is a critical component of the water and energy balances, and the number of ...
Terrestrial evapotranspiration (ET) is a central process in the climate system, is a major component...
Understanding the spatial variability in highly heterogeneous natural environments such as savannas ...
As the worlds water resources come under increasing tension due to dual stressors of climate change ...
Monitoring of water and energy fluxes is a requirement for assessment of climate and anthropogenic e...
A correct estimation of both the temporal and spatial distribution of evapotranspiration (ET) is ess...
This edition of Evapotranspiration - Remote Sensing and Modeling contains 23 chapters related to the...
Reliably and accurately quantifying evapotranspiration (ET) in a spatial and temporal domain is impo...
Studies of global hydrologic cycles, carbon cycles and climate change are greatly facilitated when. ...
Accurate estimation of spatial distributions of water (evapotranspiration) and energy fluxes is a go...
The mountains are known as the water towers of the World and they are also climate hot spots. Theref...
Thermal-infrared remote sensing of land surface temperature provides valuable information for quanti...
In semiarid areas, agricultural production is restricted by water availability; hence, efficient agr...
Being a major component of the hydrological cycle, evapotranspiration (ET) and its spatial and tempo...
Evapotranspiration (ET) is a critical component of the water and energy balances, and the number of ...
Terrestrial evapotranspiration (ET) is a central process in the climate system, is a major component...
Understanding the spatial variability in highly heterogeneous natural environments such as savannas ...
As the worlds water resources come under increasing tension due to dual stressors of climate change ...