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基于改进的双作物系数模型与Priestley-Taylor模型估算温室黄瓜蒸散量

Estimation of cucumber evapotranspiration in greenhouse based on improved dual crop coefficient model and Priestley-Taylor model

  • 摘要: 为估算温室黄瓜植株蒸腾(Tr)与土面蒸发(Eg),基于2018年春夏茬和秋冬茬温室内实测微气象数据、黄瓜作物叶面积指数(LAI)及根区土壤水分数据,对FAO-56推荐的双作物系数模型(Dual-Kc)及Priestley-Taylor(P-T)模型中参数进行修正,应用修正后的Dual-Kc和P-T模型(M-PT)估算温室黄瓜蒸散量(ETc),利用2019年春夏茬和秋冬茬实测数据对模型精度进行验证.结果表明:改进后的Dual-Kc和M-PT模型估算的温室黄瓜ETc和Tr与实测值有较好的一致性,但M-PT模型的估算误差高于Dual-Kc模型,Dual-Kc模型估算春夏茬与秋冬茬黄瓜ETc与实测值的均方根误差(RMSE)、平均绝对误差(MAE)、偏离率(Bias)和相关系数(R2)分别为0.36 mm/d, 0.28 mm/d,-0.10和0.98(春夏茬)及0.28 mm/d, 0.22 mm/d,-0.11和0.97(秋冬茬);M-PT模型的RMSE,MAE,Bias和R2分别为0.48 mm/d, 0.42 mm/d,-0.17和0.97(春夏茬)及0.41 mm/d, 0.31 mm/d,-0.24和0.95(秋冬茬).尽管M-PT模型估算误差较Dual-Kc略高,但其结构简单、所需参数较少,在温室作物蒸散量估算中更值得推广.

     

    Abstract: In order to estimate the transpiration(Tr) and soil evaporation(Eg) of cucumber plants in greenhouse conditions, based on the micro-meteorological data(measured in a greenhouse in spring-summer and autumn-winter planting seasons in 2018), cucumber crop leaf area index(LAI) and root soil moisture data in the area, the parameters in the dual crop coefficient model(Dual-Kc) and Priestley-Taylor(P-T) model recommended by FAO-56 were corrected, and the revised Dual-Kc and P-T models were applied(M-PT) to estimate greenhouse cucumber evapotranspiration(ETc). The measured data of spring-summer and autumn-winter crops in 2019 were used to verify the accuracy of the model. The results show that the ETc and Tr calculated by the improved Dual-Kc and M-PT models have a good agreement with the measured values, and the performance of the Dual-Kc model is better than that of the M-PT model. The root mean square error(RMSE), mean absolute error(MAE), deviation rate(Bias) and correlation coefficient(R~2) of the Dual-Kc model in predicting cucumber ETc are 0.36 mm/d, 0.28 mm/d,-0.10 and 0.98 for spring-summer planting season, and 0.28 mm/d, 0.22 mm/d,-0.11 and 0.97 for autumn-winter planting season, respectively. The RMSE, MAE, Bias and R~2of M-PT model are 0.48 mm/d, 0.42 mm/d,-0.17 and 0.97 for spring-summer planting season and 0.41 mm/d, 0.31 mm/d,-0.24 and 0.95 for autumn-winter planting season, respectively. Although M-PT model has a slightly higher estimation error than Dual-Kc model, its simple structure and fewer parameter requirements make it more worthy of application in the estimation of greenhouse crop evapotranspiration(ETc).

     

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