Comparison of calculation methods for determining evapotranspiration under drip irrigation

O. Zhuravlov, A. Shatkovskyi, V. V. Vasyuta, Y. O. Cherevychnyi, O. A. Marinkov, I. Kovalenko, O. Gulenko
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引用次数: 1

Abstract

The accuracy of calculation methods for determining the evapotranspiration (ET) of corn for grain under drip irrigation in the steppe of Ukraine was established. A comprehensive assessment of calculation methods for soil optimal water regime formation during different growth phases of maize plants was carried out. The accuracy of the estimated value of evapotranspiration was determined by the mean absolute percentage error (MAPE). It has been proven that the use of calculation methods without taking into account the climatic conditions of Southern Ukraine leads to a significant error in determining the actual evapotranspiration. By the Penman-Monteith method, the MAPE of 16.3-26.9% corresponds to the good and satisfactory accuracy of the chosen calculation model. Using the methods of A.M. and S.M. Alpatyev as well as D.A. Stoyko the MAPE increased to 22.2-39.7% and 20.8-29.1%, respectively, which proved their satisfactory accuracy. The calculation method of M.M. Ivanov ensured the MAPE of 48,7-76,8%; that is unsatisfactory calculation accuracy. Adapted crop coefficients Kc for the conditions of the South of Ukraine increased the accuracy of calculating ET by the Penman-Monteith method by an average of 2,2 times, D.A. Shtoyko and A.M. and S.M. Alpatiev by 1,9 and 2,2 times, and M.M. Ivanov by 4,4 times. An analysis of the MAPE using various calculation methods for determining the evapotranspiration of corn for grain under drip irrigation showed that the Penman-Monteith method provides the smallest error (MAPE = 9.1%), which corresponds to high prediction accuracy. In a wet year, the accuracy of ET determination decreases by all methods, which indicates an increase in the MAPE: by Penman-Monteith and D.A. Shtoyko - up to 11.9% and 18.7%, respectively, and the determination accuracy decreases to category “good”. When calculating using the methods of A.M. and S.M. Alpatiev and M.M. Ivanov the MAPE increased to 23,3% and 21,5%, respectively, and the accuracy of ET determination was satisfactory.
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滴灌条件下蒸散量计算方法的比较
建立了乌克兰草原滴灌条件下玉米蒸散量计算方法的准确性。对玉米不同生育期土壤最优水分状况形成的计算方法进行了综合评价。蒸散估算值的准确性由平均绝对百分比误差(MAPE)决定。已经证明,使用不考虑乌克兰南部气候条件的计算方法会导致在确定实际蒸散量时出现重大误差。通过Penman-Monteith方法,MAPE为16.3-26.9%,表明所选计算模型的精度良好且令人满意。采用A.M.和S.M. Alpatyev和D.A. Stoyko方法,MAPE分别提高到22.2 ~ 39.7%和20.8 ~ 29.1%,精度令人满意。M.M. Ivanov的计算方法保证了MAPE在48.7 ~ 76.8%之间;这是不令人满意的计算精度。乌克兰南部条件下的作物系数Kc使Penman-Monteith方法计算ET的精度平均提高了2.2倍,d.a Shtoyko和A.M.和S.M. Alpatiev分别提高了1.9和2.2倍,M.M. Ivanov提高了4.4倍。通过对不同计算方法测定滴灌条件下玉米蒸散量的MAPE进行分析,Penman-Monteith法的误差最小(MAPE = 9.1%),预测精度较高。在多雨年份,所有方法测定ET的精度都降低,表明Penman-Monteith和D.A. Shtoyko -的MAPE分别提高了11.9%和18.7%,测定精度降至“良好”类别。当采用A.M.、S.M. Alpatiev和M.M. Ivanov方法计算时,MAPE分别提高到23.3%和21.5%,ET测定的精度令人满意。
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