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首页> 外文期刊>Archives of Agronomy and Soil Science >Short-term forecasting of daily crop evapotranspiration using the 'K-c-ETo' approach and public weather forecasts
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Short-term forecasting of daily crop evapotranspiration using the 'K-c-ETo' approach and public weather forecasts

机译:使用“K-C-ETO”方法和公共天气预报的日常作物蒸发的短期预测

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Short-term forecasting of daily crop evapotranspiration (ETc) is essential for real-time irrigation management. This study proposed a methodology to forecast short-term daily ETc using the K-c-ETo' approach and public weather forecasts. Daily reference evapotranspiration (ETo) forecasts were obtained using a locally calibrated version of the Hargreaves-Samani (HS) model and temperature forecasts, while the crop coefficient (K-c) was estimated from observed daily ETo and ETc. The methodology was evaluated by comparing the daily ETc forecasts with measured ETc values from a field irrigation experiment during 2012-2014 in Yongkang Irrigation Experimental Station, China. The overall average of the statistical indices was in the range of 0.96-1.27mm d(-1) for the mean absolute error (MAE), 1.53-2.55mm d(-1) for the mean square error (MSE), 1.77-2.30mm d(-1) for the normalized mean square error (NMSE), 27.5-29.4% for the mean relative error (MRE), 0.71-0.44 for the correlation coefficient (R) and 0.46-0.05 for the mean square error skill score (MSESS). Sources of error werewere K-c estion, temperature forecasts and HS model that does not consider wind speed and humidity, and.the largesourceof error is K-c determination, which suggested that care should be taken when forecasting ETc with estimated K-c values in the study area.
机译:日常作物蒸散(ETC)的短期预测对于实时灌溉管理至关重要。本研究提出了一种使用K-C-ETO'方法和公共天气预报预测短期每日等方法。使用局部校准的Hargreaves-Samani(HS)模型和温度预测,获得每日参考蒸散(ETO)预测,而作物系数(K-C)估计每日eT​​O等。通过比较2012 - 2014年云灌在中国2012 - 2014年的现场灌溉试验中测量等值的日常等预报来评估方法。统计指数的总体平均值为0.96-1.27mm d(-1),用于平均误差(MAE),1.53-2.55mm d(-1)用于平均方误差(MSE),1.77- 2.30mm d(-1)对于归一化均方误差(nmse),27.5-29.4%,用于平均相对误差(mre),0.71-0.44,相关系数(r)和0.46-0.05的均方误差技能得分(msess)。误差源是k-c eTion,温度预测和HS模型,不考虑风速和湿度,并且误差是K-C的确定,这表明在预测时应在研究区域中的估计K-C值等。

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