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Estimation of evapotranspiration using Bowen ratio method

机译:鲍文比法估算蒸散量

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Evapotranspiration (ET) or water loss to the atmosphere is one of the most significant parts of the hydrologic cycle, and its estimation is subjected to uncertainties. Therefore, Calculation of the ET is an integral part of agricultural water management in local, regional and global water balance studies. In this study Bowen ratio method is used for measuring, deriving, and estimating input parameters for the estimation of ET for the whole cropping season for tea canopy, one month data is presented here. Results depicted the maximum and minimum estimated ET as 7.44 mmday-1and 0.12 mmday-1respectively. The overall estimated ET for the whole month was 3.423633 mmday-1. The estimated ET will be compared and calibrated against direct ET estimation method (i.e. eddy covariance) for the whole cropping season and further predictions will be provided about the implementation of this method for other crops as well.
机译:蒸散(ET)或水分流失到大气中是水文循环最重要的部分之一,其估算存在不确定性。因此,在局部,区域和全球水平衡研究中,ET的计算是农业水管理的组成部分。在这项研究中,Bowen比率法用于测量,推导和估计输入参数,以估算茶冠层整个种植季节的ET,此处提供一个月的数据。结果描述的最大和最小估计ET分别为7.44 mmday-1和0.12 mmday-1。整个月的估计总ET为3.423633 mmday-1。估计的ET将与整个作物季节的直接ET估计方法(即涡度协方差)进行比较和校准,并将对该方法在其他作物上的实施提供进一步的预测。

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