The triangle method has been applied to derive a weekly indicator of evaporative fraction on vegetated areas in a temperate region in Northern Italy. Daily MODIS Aqua Land Surface Temperature (MYD11A1) data has been combined with air temperature maps and 8-day composite MODIS NDVI (MOD13Q1/MYD13Q1) data to estimate the Evaporative Fraction (EF) at 1 km resolution, on a daily basis. Measurements at two eddy covariance towers located within the study area have been exploited to assess the reliability of satellite based EF estimations as well as the robustness of input data. Weekly syntheses of the daily EF indicator (EFw) were then derived at regional scale for the years 2010, 2011 and 2012 as a proxy of overall surface moisture condition. EF...
Satellite-derived evapotranspiration anomalies and normalized difference vegetation index (NDVI) pro...
The Penman–Monteith (P-M) model has been widely used to estimate actual evapotranspiration (ET). How...
Irrigation according to reliable estimates of crop water requirements (CWR) is one of the key strate...
The triangle method has been applied to derive a weekly indicator of evaporative fraction on vegetat...
This work presents a simple, cost-effective, and operational approach to monitor crop water requirem...
Time-varying crop coefficients (Kc) can be obtained from remotely sensed data and combined with dail...
The most commonly used normalized difference vegetation index (NDVI) from remote sensing often fall ...
In this study, spatially distributed estimates of regional actual evapotranspiration (ET) were obtai...
Water use efficiency in agriculture can be improved by implementing advisory systems that support on...
In this study, accurate estimates of daily actual evapotranspiration, ETa, were obtained based on th...
Routine information on regional evapotranspiration (ET) and dryness index is essential for agricultu...
Terrestrial evapotranspiration is a critical process for the energy and hydrologic partitioning at t...
Water availability is one of the limiting factors to crop growth in arid and semi-arid zones. Shorta...
Satellite-derived evapotranspiration anomalies and normalized difference vegetation index (NDVI) pro...
The Penman–Monteith (P-M) model has been widely used to estimate actual evapotranspiration (ET). How...
Irrigation according to reliable estimates of crop water requirements (CWR) is one of the key strate...
The triangle method has been applied to derive a weekly indicator of evaporative fraction on vegetat...
This work presents a simple, cost-effective, and operational approach to monitor crop water requirem...
Time-varying crop coefficients (Kc) can be obtained from remotely sensed data and combined with dail...
The most commonly used normalized difference vegetation index (NDVI) from remote sensing often fall ...
In this study, spatially distributed estimates of regional actual evapotranspiration (ET) were obtai...
Water use efficiency in agriculture can be improved by implementing advisory systems that support on...
In this study, accurate estimates of daily actual evapotranspiration, ETa, were obtained based on th...
Routine information on regional evapotranspiration (ET) and dryness index is essential for agricultu...
Terrestrial evapotranspiration is a critical process for the energy and hydrologic partitioning at t...
Water availability is one of the limiting factors to crop growth in arid and semi-arid zones. Shorta...
Satellite-derived evapotranspiration anomalies and normalized difference vegetation index (NDVI) pro...
The Penman–Monteith (P-M) model has been widely used to estimate actual evapotranspiration (ET). How...
Irrigation according to reliable estimates of crop water requirements (CWR) is one of the key strate...