In this study, the performance of nine mass transfer-based equations for estimating reference evapotranspiration (ET0) was statistically analyzed in comparison to widely accepted Food and Agriculture Organization Penman-Monteith method (FAO-56 PM) model forsub-humid Udham Singh Nagar district of Uttarakhand. The higher values of Agreement index, coefficient of determination, correlation coefficient; and lowercalculated values of Root Mean Square Error, Mean Bias Error, Maximum Absolute Error, Percentage Error and Standard Error of Estimate between ET0 values obtained with WMO and FAO-56 PM ET0 methods observed on dailyand monthly basis confirms acceptability of WMO method. The ratio of ET0 method/ET0 FAO-56 PM was found best (almost near to...
The exact estimation of crop evapotranspiration containing reference or potential evapotranspiration...
Estimation of evapotranspiration is necessary for planning, design and irrigation design and water r...
In order to compare different methods of calculating evapotranspiration reference (ET0) with the sta...
Proper assessment of reference evapotranspiration (ET0) is necessary for pastoral activity and water...
Accurate estimation of potential evapotranspiration is necessary step in water resources management....
The study planed to identify a suitable alternative to the FAO-56 Penman-Monteith (FAO56PM) equation...
AbstractThe study planed to identify a suitable alternative to the FAO-56 Penman-Monteith (FAO56PM) ...
The reference crop evapotranspiration (ET0) was estimated for three locations of Bangladesh using th...
ABSTRACT: Agricultural planning relying on evapotranspiration suffers due to inaccuracy in its estim...
The study was carried out to select best alternative method for the estimation of reference evapotra...
FAO-56-Penman-Monteith is regarded as a standard method worldwide for calculation of ET. However due...
Preciseestimation of evapotranspiration is an importantstep in the field of water resource managemen...
This paper investigates the evaluation and inter comparison of evapotranspiration models with data f...
Evapotranspiration is one of the major components of the hydrologic cycle is highly important in stu...
The use of empirical agrometeorological models that can be adjusted to the climatic conditions of di...
The exact estimation of crop evapotranspiration containing reference or potential evapotranspiration...
Estimation of evapotranspiration is necessary for planning, design and irrigation design and water r...
In order to compare different methods of calculating evapotranspiration reference (ET0) with the sta...
Proper assessment of reference evapotranspiration (ET0) is necessary for pastoral activity and water...
Accurate estimation of potential evapotranspiration is necessary step in water resources management....
The study planed to identify a suitable alternative to the FAO-56 Penman-Monteith (FAO56PM) equation...
AbstractThe study planed to identify a suitable alternative to the FAO-56 Penman-Monteith (FAO56PM) ...
The reference crop evapotranspiration (ET0) was estimated for three locations of Bangladesh using th...
ABSTRACT: Agricultural planning relying on evapotranspiration suffers due to inaccuracy in its estim...
The study was carried out to select best alternative method for the estimation of reference evapotra...
FAO-56-Penman-Monteith is regarded as a standard method worldwide for calculation of ET. However due...
Preciseestimation of evapotranspiration is an importantstep in the field of water resource managemen...
This paper investigates the evaluation and inter comparison of evapotranspiration models with data f...
Evapotranspiration is one of the major components of the hydrologic cycle is highly important in stu...
The use of empirical agrometeorological models that can be adjusted to the climatic conditions of di...
The exact estimation of crop evapotranspiration containing reference or potential evapotranspiration...
Estimation of evapotranspiration is necessary for planning, design and irrigation design and water r...
In order to compare different methods of calculating evapotranspiration reference (ET0) with the sta...