Accurate measurement and estimation of crop evapotranspiration (ET) plays an important role in understanding field soil water cycle and managing water-saving irrigation in the arid regions. This study compares three methods for estimating ET: field Water Balance (WB), Eddy Covariance (EC) and Bowen Ratio-Energy Balance (BREB). The experiment was conducted in a vineyard in the arid desert regions of northwest China. Results indicate that the three methods provided similar estimate of total ET. Compared to total ET measured by WB (ETWB) during the whole growing stage, total ET estimated by EC (ETEC) was 1.57% lower, and total ET estimated by BREB (ETBREB) was 5.19% higher. Variations of ETEC and ETBREB are similar at hourly or daily timescale...
Measuring and counting reference crops evapotranspiration (ET0) accurately is of great importance fo...
Quantification of the components of evapotranspiration (ET) is key to designing management strategie...
Evaporation from the soil surface (E) can be a significant source of water loss in arid areas. In sp...
Accurate measurement and estimation of crop evapotranspiration (ET) plays in important in understand...
Agricultural water requirement in arid and semi-arid environments represents an important fraction o...
Grapevines are extensively grown in the semiarid and arid regions, but little information is availab...
Accurate determination of evapotranspiration (ET) has tremendous potential in guiding irrigation and...
Two Bowen ratio-energy balance (BREB) systems for measuring evapotranspiration (ET) under wet and dr...
The assessment of the water needs for a specific crop has a fundamental importance in the management...
Understanding the regulation of ecosystem ET is crucial to comprehend present and potential future v...
Evapotranspiration (ET) is an important component of the surface energy balance and water cycle, esp...
Evapotranspiration (ET) is critical for ecosystem protection and water services, especially in the m...
Evapotranspiration (ET) is an important component in the water budget and used extensively in water ...
Different methods for assessing evapotranspiration (ET) can significantly affect the performance of ...
Accurate continuous daily evapotranspiration (ET) at the field scale is crucial for allocating and m...
Measuring and counting reference crops evapotranspiration (ET0) accurately is of great importance fo...
Quantification of the components of evapotranspiration (ET) is key to designing management strategie...
Evaporation from the soil surface (E) can be a significant source of water loss in arid areas. In sp...
Accurate measurement and estimation of crop evapotranspiration (ET) plays in important in understand...
Agricultural water requirement in arid and semi-arid environments represents an important fraction o...
Grapevines are extensively grown in the semiarid and arid regions, but little information is availab...
Accurate determination of evapotranspiration (ET) has tremendous potential in guiding irrigation and...
Two Bowen ratio-energy balance (BREB) systems for measuring evapotranspiration (ET) under wet and dr...
The assessment of the water needs for a specific crop has a fundamental importance in the management...
Understanding the regulation of ecosystem ET is crucial to comprehend present and potential future v...
Evapotranspiration (ET) is an important component of the surface energy balance and water cycle, esp...
Evapotranspiration (ET) is critical for ecosystem protection and water services, especially in the m...
Evapotranspiration (ET) is an important component in the water budget and used extensively in water ...
Different methods for assessing evapotranspiration (ET) can significantly affect the performance of ...
Accurate continuous daily evapotranspiration (ET) at the field scale is crucial for allocating and m...
Measuring and counting reference crops evapotranspiration (ET0) accurately is of great importance fo...
Quantification of the components of evapotranspiration (ET) is key to designing management strategie...
Evaporation from the soil surface (E) can be a significant source of water loss in arid areas. In sp...