高级检索+

六种冠层阻力模型在冬小麦蒸散估算中的应用

Application of six canopy resistance models for estimating winter wheat evapotranspiration

  • 摘要: 蒸散量是农田水循环中水分损失的主要途径,其准确估算对节水灌溉具有重要意义。单源的Penman-Monteith (P-M)模型是最常用的蒸散量估算方法,但模型中冠层阻力的合理参数化一直是研究中的难点。该研究选取常用6种冠层阻力模型,使用北京顺义2 a(2020年和2021年)的波文比实测结果,分析不同模型进行冬小麦冠层阻力及蒸散估算的可行性。结果表明:1)无参数校正条件下,6种模型均低估了冬小麦冠层阻力,同时高估了蒸散量。其中,Todorovic模型(TD)的普适性最好,其模拟的冠层阻力、蒸散量与实测值的R2都在0.605及以上;耦合的冠层阻力模型(CO模型)普适性最差,冠层阻力、蒸散量与实测值的R2分别为0.113、0.046;2)进一步使用2021年的试验数据进行模型参数校正、2020年的数据进行验证,发现校正后的JA、CO、GA、KP及FAO56-PM模型计算的冠层阻力和蒸散量与实测值的一致性大幅提高。除JA模型低估冠层阻力外,其余均高估冠层阻力、低估蒸散量。其中KP模型模拟的冠层阻力和蒸散量效果最好,R2均在0.907及以上,而其余5种模型估算精度也较好。6种模型的估算精度排序为KP、GA、TD、FAO56-PM、CO、JA。综上,所评价的模型校正后均可作为P-M模型的冠层阻力输入来估算冬小麦蒸散量,但TD 模型不需要参数校正,在数据不足时可作为首选;而KP模型参数较少,校正后拟合精度最高,在数据充足时可作为首选。研究结果对华北地区使用P-M一步法计算冬小麦蒸散量具有重要价值。

     

    Abstract: Abstract: Evapotranspiration (ET) is the main way of water loss in the farmland water cycle in precision agriculture. An accurate ET estimation is of great significance for water-saving irrigation. Extensive studies have been carried out on ET measurement and simulation in recent years. Among them, the single source Penman-Monteith (P-M) model has been one of the most commonly-used models. But, a major challenge still remained on the accurate parameterization of canopy resistance in the P-M. In this study, six commonly-used canopy resistance models were selected to test the simulated canopy resistance with the P-M for the direct estimation of winter wheat ET. The P-M simulated ET was compared with the measured values of Bowen ratio over the wheat canopy in Shunyi District, Beijing for two years (2020 and 2021). The results showed that: 1) The six models underestimated the canopy resistance of winter wheat, but overestimated ET with the original parameters. Among them, the Todorovic model (TD) performed the best, where the R2 between the measured and simulated for the canopy resistance and ET were above 0.605, the Mean Bias Error (MBE) of -82.8 s/m and 10.4 W/m2, respectively, with the Root Mean Square Error (RMSE) of 254.4 s/m and 33.5 W/m2. The coupled canopy resistance model (CO model) performed the worst, where the R2 for the canopy resistance and ET were 0.113 and 0.046, respectively, with the MBE of -236.4 s/m and 97.4 W/m2, as well as the corresponding RMSE of 373.8 s/m and 147.9 W/m2, respectively. The RMSE was ranked as a decreased order by TD, FAO56-PM, Katerji Perrier (KP), Garc?á - Santos (GA), Jarvis (JA), and CO. 2) Further parameter calibration with the data of 2021 and the verification with data of 2020 showed that there was greatly improved performance in the simulated wheat canopy resistance and ET by JA, CO, GA, KP, and FAO56-PM. Except the JA model underestimated the wheat canopy resistance, the others overestimated the canopy resistance and underestimated the wheat ET. Specifically, the KP obtained the best prediction, where the R2 values for the canopy resistance and ET were larger than 0.907, with the respective MBE of 41.1 s/m and -14.7 W/m2, and the corresponding RMSE of 94.0 s/m and 21.5 W/m2, respectively. The performance of the other five models was also feasible, where the R2 values for the simulated wheat canopy resistance and ET were larger than 0.641, the MBE ranging -25.4-24.0 s/m and -11.7-7.2 W/m2, respectively, with the RMSE of 76.8-265.2 s/m and 22.2-26.4 W/m2. The performance was then ranked as a decreased order by KP, GA, TD, FAO56-PM, CO and JA. 3) All six models can be used to predict the rs that are needed by the P-M model for the estimation of the winter wheat evapotranspiration. Nevertheless, the TD model obtained the best wheat rs and ET estimates, even without the local calibration. Thus the TD model can be the first choice in the data-lacking environment. The KP model also needed only a few parameters for the highest accuracy after calibration, particularly for the data-sufficient environment. The findings can provide a better guide application of the P-M's one-step approach to estimate the winter wheat ET in the region of North China.

     

/

返回文章
返回