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Benchmarking test of empirical root water uptake models

机译:经验根系吸水模型的基准测试

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Detailed physical models describing root water uptake (RWU) are an important tool for the prediction of RWU and crop transpiration, but the hydraulic parameters involved are hardly ever available, making them less attractive for many studies. Empirical models are more readily used because of their simplicity and the associated lower data requirements. The purpose of this study is to evaluate the capability of some empirical models to mimic the RWU distribution under varying environmental conditions predicted from numerical simulations with a detailed physical model. A review of some empirical models used as sub-models in ecohydrological models is presented, and alternative empirical RWU models are proposed. All these empirical models are analogous to the standard Feddes model, but differ in how RWU is partitioned over depth or how the transpiration reduction function is defined. The parameters of the empirical models are determined by inverse modelling of simulated depth-dependent RWU. The performance of the empirical models and their optimized empirical parameters depends on the scenario. The standard empirical Feddes model only performs well in scenarios with low root length density iR/i, i.e. for scenarios with low RWU qcompensation/q. For medium and high iR/i, the Feddes RWU model cannot mimic properly the root uptake dynamics as predicted by the physical model. The Jarvis RWU model in combination with the Feddes reduction function (JMf) only provides good predictions for low and medium iR/i scenarios. For high iR/i, it cannot mimic the uptake patterns predicted by the physical model. Incorporating a newly proposed reduction function into the Jarvis model improved RWU predictions. Regarding the ability of the models to predict plant transpiration, all models accounting for compensation show good performance. The Akaike information criterion (AIC) indicates that the Jarvis?(2010) model (JMII), with no empirical parameters to be estimated, is the qbest model/q. The proposed models are better in predicting RWU patterns similar to the physical model. The statistical indices point to them as the best alternatives for mimicking RWU predictions of the physical model.
机译:描述根部水分吸收(RWU)的详细物理模型是预测RWU和农作物蒸腾作用的重要工具,但是涉及的水力参数几乎无法获得,因此对许多研究而言都缺乏吸引力。由于经验模型简单且相关的数据需求较低,因此更易于使用。这项研究的目的是评估一些经验模型在具有详细物理模型的数值模拟所预测的变化环境条件下模拟RWU分布的能力。提出了一些作为生态水文模型子模型的经验模型的综述,并提出了替代的经验RWU模型。所有这些经验模型都类似于标准的Feddes模型,但是在RWU深度上划分方式或蒸腾减少函数的定义方式不同。经验模型的参数是通过对依赖于深度的模拟RWU进行逆建模来确定的。经验模型的性能及其优化的经验参数取决于场景。标准的经验Feddes模型仅在根长度密度 R 低的情况下(即,在RWU 补偿低的情况下)表现良好。对于中等和较高的 R ,Feddes RWU模型无法正确模拟物理模型所预测的根系吸收动力学。 Jarvis RWU模型与Feddes缩减功能(JMf)结合使用只能为中低 R 场景提供良好的预测。对于高 R ,它无法模拟物理模型预测的吸收模式。将最新提出的归约函数纳入Jarvis模型可改善RWU预测。关于模型预测植物蒸腾能力,所有补偿模型均显示出良好的性能。 Akaike信息标准(AIC)表示,没有经验参数可供估计的Jarvis?(2010)模型(JMII)是最佳模型。所提出的模型在预测与物理模型相似的RWU模式方面效果更好。统计指标指出,它们是模仿物理模型的RWU预测的最佳选择。

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