Continuous daily evapotranspiration (ET) monitoring at the field-scale is crucial for water resource management in irrigated agricultural areas in arid regions. Here, an integrated framework for daily ET, with the required spatiotemporal resolution, is described. Multi-scale surface energy balance algorithm evaluations and a data fusion algorithm are combined to optimally exploit the spatial and temporal characteristics of image datasets, collected by the advanced space-borne thermal emission reflectance radiometer (ASTER) and the moderate resolution imaging spectroradiometer (MODIS). Through combination with a linear unmixing-based method, the spatial and temporal adaptive reflectance fusion model (STARFM) is modified to generate high-reso...
ABSTRACT. Evapotranspiration (ET) is an essential component of the water balance and a major consump...
Evapotranspiration (ET) is a significant consumer of irrigation water and precipitation on cropland....
The quantification of land surface evapotranspiration (ET) at daily or longer time scales is of grea...
Continuous monitoring of daily evapotranspiration (ET) at field scale can be achieved by combining t...
AbstractContinuous monitoring of daily evapotranspiration (ET) at field scale can be achieved by com...
Evapotranspiration (ET) represents crop water use and is a key indicator of crop health. Accurate es...
Continuous high spatio-temporal resolution monitoring of evapotranspiration (ET) is critical for wat...
Continuous evapotranspiration (ET) data with high spatial resolution are crucial for water resources...
Evapotranspiration (ET) plays an essential role in agricultural water resource management. Understan...
Evapotranspiration (ET) plays an essential role in agricultural water resource management. Understan...
Thermal remote sensing methods for mapping evapotranspiration (ET) exploit the physical interconnect...
Irrigation of agricultural land is the main water consumer in the arid and semiarid regions. The acc...
Accurate continuous daily evapotranspiration (ET) at the field scale is crucial for allocating and m...
Evapotranspiration (ET) is an essential component of the water balance. Any attempt to improve water...
International audienceEvapotranspiration (ET) estimates are particularly needed for monitoring avail...
ABSTRACT. Evapotranspiration (ET) is an essential component of the water balance and a major consump...
Evapotranspiration (ET) is a significant consumer of irrigation water and precipitation on cropland....
The quantification of land surface evapotranspiration (ET) at daily or longer time scales is of grea...
Continuous monitoring of daily evapotranspiration (ET) at field scale can be achieved by combining t...
AbstractContinuous monitoring of daily evapotranspiration (ET) at field scale can be achieved by com...
Evapotranspiration (ET) represents crop water use and is a key indicator of crop health. Accurate es...
Continuous high spatio-temporal resolution monitoring of evapotranspiration (ET) is critical for wat...
Continuous evapotranspiration (ET) data with high spatial resolution are crucial for water resources...
Evapotranspiration (ET) plays an essential role in agricultural water resource management. Understan...
Evapotranspiration (ET) plays an essential role in agricultural water resource management. Understan...
Thermal remote sensing methods for mapping evapotranspiration (ET) exploit the physical interconnect...
Irrigation of agricultural land is the main water consumer in the arid and semiarid regions. The acc...
Accurate continuous daily evapotranspiration (ET) at the field scale is crucial for allocating and m...
Evapotranspiration (ET) is an essential component of the water balance. Any attempt to improve water...
International audienceEvapotranspiration (ET) estimates are particularly needed for monitoring avail...
ABSTRACT. Evapotranspiration (ET) is an essential component of the water balance and a major consump...
Evapotranspiration (ET) is a significant consumer of irrigation water and precipitation on cropland....
The quantification of land surface evapotranspiration (ET) at daily or longer time scales is of grea...