Abstract:
Evapot
ranspi
ration (ET) is critical for energy and water balance in agricultu
ral systems. Accu
rate estimation or measurement of ET is therefore important in improving water use efficiency and optimizing the structure of regional water use. Canopy resistance is one of the most important variables in the estimation of ET. The accu
racy of simulation of the response process of canopy resistance to environmental variables is critically important for crop ET research. A convenient approach to simulate the response process of canopy resistance to multiple factors is based on the relationship between measured latent heat, climatic variables and by using the modified Penman-Monteith (P-M) equation. However, this method has certain limitations in some p
ractical applications due to the lack of a few effective pa
rameters. Another approach is to construct empirical and semi-empirical models using multiple factors (such as the Irmak model) based on measured data combined with the rear
ranged P-M equation. Based on canopy resistance values calculated by the rear
ranged P-M equation and on maize data (for the period May to September 2012) collected from the three eddy covariance observation stations in Heihe River Basin, this study constructed Irmak model taking into account the effect of atmospheric CO
2 concent
ration of half-hourly and daily time-steps to simulate the response processes of maize to environmental variables such as net
radiation (
Rn), air tempe
rature (
Ta), leaf area index (LAI), relative humidity (RH), wind speed (
U3), aerodynamic resistance (
ra), effective soil water content (
θ) and atmospheric CO
2 concent
ration. In the study, the performance of the two Irmak models were tested with measured values of latent heat from the eddy covariance systems of the other two verification points. Besides, the sensitivity of environmental variables was analyzed. The results indicated that the improved Irmak model which took into account the effect of atmospheric CO
2 concent
ration well estimated canopy resistance and ET. The coefficients of determination (
R2) for canopy resistance and ET were respectively 0.76 and 0.95 for the calib
ration phase, with root mean square errors (RMSE) of 33.1 s·m
-1 and 34.5 W·m
-2. Meanwhile,
R2 for canopy resistance and ET were respectively 0.68 and 0.90 for the validation phase, with RMSE of 63.2 s·m
-1 and 49.0 W·m
-2. The two verification points showed that the improved Irmak model had a good performance and strong regional applicability and spatial portability. The model also simulated the response processes of canopy resistance to environmental variables and reflected the effect of the variations in atmospheric CO
2 concent
ration on ET. Sensitivity analysis of the improved Irmak model showed that canopy and ET were the most sensitive to net
radiation and relative humidity, followed by air tempe
rature, leaf area index and atmospheric CO
2 concent
ration. The improved Irmak model used in this study was applicable in estimating crop water consumption and the accu
racy of ET of maize, in providing scientific basis for improvements in water use efficiency and in optimizing the structure of regional water use under increased future atmospheric CO
2 concent
ration.