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COMPARISON OF SEBAL-BASED EVAPOTRANSPIRATION WITH LYSIMETERIC DATA

机译:酶促数据的Sebal基蒸散的比较

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There are several algorithms for estimation of crop evapotranspiration such as SEBAL (Surface Energy Balance Algorithm for Land). In this study, SEBAL was used for estimation and evaluation of agricultural crop evapotranspiration by using of MODIS, NOAA, and ASTER imaginary and meteorological data of Kerman province and consequently results were compared with lysimeteric data. Due to hot and dry climate of the study area, optimum value of L (soil adjustment factor) had to be determined. Results show that increasing of L causes increasing of estimated evapotranspiration and minimum errors occurred when L equals to 1. In this case, RMSE was 0.29 and 0.76 by the use of MOSIS and NOAA imaginary respectively. Relative error of evapotranspiration estimation by SEBAL from MODIS, NOAA and ASTER images are 10%, 13% and 3.57% respectively. Errors are introduced by the difference in time of irrigation and different characteristics of cultivated plant in lysimeter data, adjacent farms, around area and interpolation of hourly meteorological data.
机译:存在若干算法,用于估计诸如Sebal(地表能量平衡算法的茶叶蒸发)。在本研究中,通过使用Modis,NOAA和肯尼斯省的紫外线假想和气象数据,SEBAL用于估算和评估农业作物蒸发,因此与尿少数表数据进行了结果。由于研究区域的炎热和干燥气候,必须确定L(土壤调节因子)的最佳值。结果表明,L的原因估计蒸散和最小误差的增大而增大时L等于1。在这种情况下发生,RMSE分别假想为0.29和0.76通过使用MOSIS和NOAA的。 Sebal从Modis,NOAA和ASTER图像估算的相对误差分别为10%,13%和3.57%。误差是通过灌溉时间差异和培养植物的不同特征引入植物,邻近农场,周围区域和每小时气象数据的插值。

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