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首页> 外文期刊>Journal of Hydrology >Comparison of the use of a physical-based model with data assimilation and machine learning methods for simulating soil water dynamics
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Comparison of the use of a physical-based model with data assimilation and machine learning methods for simulating soil water dynamics

机译:基于物理模型与模拟土壤水动力学的数据同化和机器学习方法的使用比较

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Soil moisture plays a critical role as an essential component of the global water resources by regulating mass and energy exchange between land surface and atmosphere. Quantification of these exchange processes requires accurate characterization and simulation of soil water movement. Physically-based models (PBMs) and machine learning methods (MLMs) can both be used in soil moisture simulation. However, their performances in soil water simulation have only been compared in a limited number of cases. Moreover, almost all of them are conducted in field studies each with fixed soil, initial condition, and boundary condition. Here, we developed three artificial neural network (ANN) frameworks, and made clearer and more systematic comparisons between them and a PBM-Ross numerical model solving Richards equation and parameter estimation using a data assimilation approach (iterative ensemble smoother, Ross-IES) in synthetic and real-world conditions. Compared with the ANNs, Ross-IES is more significantly affected by physical model uncertainties such as soil heterogeneity, initial and boundary conditions, while both methods are affected by observation noise. For Ross-IES, the errors from boundary conditions and hydraulic parameter conceptualization are found to be more prominent than that of observation noise and therefore are suggested to be identified first. Meanwhile, the ANNs have difficulty in simulating the peaks and troughs of the soil water time series as well as in situations where the soil moisture is constantly saturated. ANNs yield a superior simulation when the nonlinear relationship between the response variables and driving data is weak, while the performance of Ross-IES is governed by the prior soil hydraulic information. In addition, Ross-IES approach requires much higher computational cost than the ANNs. ANN-MS performs best among the three ANN-based machine learning models and demonstrates great data mining ability and robustness against overfitting.
机译:通过调节土地表面和大气之间的质量和能量交换,土壤水分作为全球水资源的重要组成部分。这些交换过程的量化需要准确表征和模拟土壤水运动。基于物理的模型(PBMS)和机器学习方法(MLMS)都可以用于土壤湿度模拟。然而,它们在土壤水模拟中的性能仅在有限数量的情况下进行了比较。此外,几乎所有这些都在现场研究中进行,每个研究都有固定的土壤,初始条件和边界条件。在这里,我们开发了三个人工神经网络(ANN)框架,并在它们之间进行了更清晰,更系统的比较,并使用数据同化方法(迭代集合更顺畅,ROSS-IES)解决了理查兹方程和参数估计的PBM-ROSS数值模型综合性和现实世界的条件。与ANNS相比,ROSS-IES更为显着地受到物理模型不确定性的影响,例如土壤异质性,初始和边界条件,而两种方法受观察噪声的影响。对于ROSS-IE,发现来自边界条件和液压参数概念化的误差比观察噪声更加突出,因此建议首先识别。同时,ANNS难以模拟土壤水时间序列的峰和槽以及土壤水分不断饱和的情况。当响应变量与驾驶数据之间的非线性关系较弱时,ANNS产生卓越的模拟,而ROSS-IE的性能受到现有土壤液压信息的管辖。此外,ROSS-IES方法需要比ANNS更高的计算成本。 Ann-MS在三个基于Ann的机器学习模型中表现最佳,并展示了巨大的数据挖掘能力和对过度装备的鲁棒性。

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