摘要
为有效提高中国西北地区Rs预报精度,选取西北地区11个代表性气象站点1959—2015年逐日气象数据,评价了4种基于日照时数的Rs计算模型(Angstrom-Prescott,Ogelman,Bahel和Louche模型)和2种基于温度的Rs计算模型(Hargreaves和Bristow-Campbell模型)在西北地区4个分区(温带大陆性高温干旱区、温带大陆性干旱区、高原大陆性半干旱区和温带季风半干旱区)的适用性.结果表明:6种模型在西北地区的Rs模拟值与实测值均在P<0.001水平具有统计学意义;基于日照时数的Rs计算模型(R2介于0.901~0.903)精度高于基于温度的模型(R2介于0. 695~0. 719);其中,基于日照时数的模型中Bahel模型的精度最高,其R2,MAE,MRE,RMSE和NSE分别为0.903,1.624 MJ/(m2·d),15.7%,2.298 MJ/(m2·d)和0.902;基于温度的模型中Bristow-Campbell模型精度最高,其值分别为0.719,2.851 MJ/(m2·d),30.7%,3.959 MJ/(m2·d)和0. 713.因此,为有效提高西北地区Rs日值和月值预报精度,在仅有温度资料时推荐使用Bristow-Campbell模型,在仅有日照时数资料时推荐使用Bahel模型.
To effectively improve the prediction accuracy of Rsin Northwest China,the daily climate data collected from 11 representive meteorological stations during 1959—2015 were used to estimate Rs.Four kinds of sunshine-based models(Angstrom-Prescott,Ogelman,Bahel and Louche models)and two kinds of temperature-based models(Hargreaves and Bristow-Campbell models) were evaluated in four sub-zones,which are the temperate continental high temperature-arid zone,the temperate continental arid zone,the plateau continental semiarid zone and the temperate monsoon semiarid zone.The results show that the estimate Rsresults of each model has a significant correlation with the measured value at the 0.001 level.Generally,the applicability of sunshine-based model(with R2 ranging from 0.901 to 0.903) is better than that of temperature-based model(with R2 ranging from 0.695 to 0.719).Among the 4 sunshine-based models,Bahel model shows the best performance,with R2 of0.903,MAE of 1.624 MJ/(m2·d),MRE of 15.7%,RMSE of 2.298 MJ/(m2·d) and NSE of0.902.The most accurate temperature-based model is Bristow-Campbell model,with R2 of 0.719,MAE of 2.851 MJ/(m2·d),MRE of 30.7%,RMSE of 3.959 MJ/(m2·d) and NSE of 0.713.Overall,the Bahel model is recommended to estimate daily and monthly Rswhen only the sunshine duration data are avai-lable in Northwest China and the Bristow-Campbell model is recommended to estimate Rswhen only temperature data are available.
引文
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