In this study, the performance of three empirical methods for estimating reference evapotranspiration (ET0): Makkink (Mak) and Priestley-Taylor (PT) (radiation-based) and Hargreaves-Samani (HARG) (temperature-based) were assessed in semi-and regions. The values of ET0 derived using these three methods were compared to those estimated using the reference FAO Penman-Monteith (FAO-PM) method under semi-arid conditions of the Tensift basin (central of Morocco) and the Yaqui Valley (Northwest Mexico). The results showed that the HARG method is the best one to estimate ET0 over both semi-and test sites. Conversely, the performance of the other two empirical methods was poor except under humid conditions. However when the parameters alpha and C-m ...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
Evapotranspiration is a key variable for hydrologic, climatic, agricultural, and environmental studi...
In this study, the performance of three empirical methods for estimating reference evapotranspiratio...
Reference evapotranspiration (ETo) is an important parameter for climatological, hydrological and ag...
The standard FAO Penman–Monteith (PM-ETo) method for computing the reference evapotranspiration (ET...
Monthly data records of 40 Iranian stations distributed over the country, for the period 1971–2005, ...
In this paper attempt is made to estimate reference evapotranspiration (ETo) from standard meteorolo...
Reference crop evapotranspiration (ETo) is among the most important components of the hydrologic cyc...
Evapotranspiration (ET) is an important component of the hydrologic cycle, especially for irrigated ...
This paper reports the results of using three empirical methods (Makkink, Priestley-Taylor and Hargr...
The study was carried out to select best alternative method for the estimation of reference evapotra...
In this study, two site-specific solar radiation (Rs) and net radiation (Rn) based equations for est...
Evapotranspiration (ET) is of great importance in many disciplines, including irrigation system des...
Reliable estimation of evapotranspiration (ET) is important for the purpose of water resources plann...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
Evapotranspiration is a key variable for hydrologic, climatic, agricultural, and environmental studi...
In this study, the performance of three empirical methods for estimating reference evapotranspiratio...
Reference evapotranspiration (ETo) is an important parameter for climatological, hydrological and ag...
The standard FAO Penman–Monteith (PM-ETo) method for computing the reference evapotranspiration (ET...
Monthly data records of 40 Iranian stations distributed over the country, for the period 1971–2005, ...
In this paper attempt is made to estimate reference evapotranspiration (ETo) from standard meteorolo...
Reference crop evapotranspiration (ETo) is among the most important components of the hydrologic cyc...
Evapotranspiration (ET) is an important component of the hydrologic cycle, especially for irrigated ...
This paper reports the results of using three empirical methods (Makkink, Priestley-Taylor and Hargr...
The study was carried out to select best alternative method for the estimation of reference evapotra...
In this study, two site-specific solar radiation (Rs) and net radiation (Rn) based equations for est...
Evapotranspiration (ET) is of great importance in many disciplines, including irrigation system des...
Reliable estimation of evapotranspiration (ET) is important for the purpose of water resources plann...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
In semi-arid regions, the largest portion of rainfall is lost as evapotranspiration (ET). Therefore,...
Evapotranspiration is a key variable for hydrologic, climatic, agricultural, and environmental studi...