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首页> 外文期刊>Journal of Hydrology >Assessing artificial neural networks and statistical methods for infilling missing soil moisture records
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Assessing artificial neural networks and statistical methods for infilling missing soil moisture records

机译:评估人工神经网络和统计方法以填补缺失的土壤水分记录

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摘要

Soil moisture information is critically important for water management operations including flood forecasting, drought monitoring, and groundwater recharge estimation. While an accurate and continuous record of soil moisture is required for these applications, the available soil moisture data, in practice, is typically fraught with missing values. There are a wide range of methods available to infilling hydrologic variables, but a thorough inter-comparison between statistical methods and artificial neural networks has not been made. This study examines 5 statistical methods including monthly averages, weighted Pearson correlation coefficient, a method based on temporal stability of soil moisture, and a weighted merging of the three methods, together with a method based on the concept of rough sets. Additionally, 9 artificial neural networks are examined, broadly categorized into feedforward, dynamic, and radial basis networks. These 14 infilling methods were used to estimate missing soil moisture records and subsequently validated against known values for 13 soil moisture monitoring stations for three different soil layer depths in the Yanco region in southeast Australia. The evaluation results show that the top three highest performing methods are the nonlinear autoregressive neural network, rough sets method, and monthly replacement. A high estimation accuracy (root mean square error (RMSE) of about 0:03 m3=m3) was found in the nonlinear autoregressive network, due to its regression based dynamic network which allows feedback connections through discrete-time estimation. An equally high accuracy (0.05 m3=m3 RMSE) in the rough sets procedure illustrates the important role of temporal persistence of soil moisture, with the capability to account for different soil moisture conditions.
机译:土壤水分信息对于水管理工作(包括洪水预报,干旱监测和地下水补给估算)至关重要。虽然这些应用需要准确连续的土壤水分记录,但实际上,可用的土壤水分数据通常充满缺失值。填充水文变量的方法多种多样,但统计方法与人工神经网络之间没有进行全面的比较。这项研究研究了5种统计方法,包括月平均值,加权Pearson相关系数,一种基于土壤水分的时间稳定性的方法以及三种方法的加权合并以及一种基于粗糙集的方法。此外,还检查了9个人工神经网络,将其大致分为前馈,动态和径向基网络。这14种填充方法用于估计缺失的土壤水分记录,随后针对澳大利亚东南部Yanco地区三种不同土壤层深度的13个土壤水分监测站的已知值进行了验证。评估结果表明,性能最高的三种方法是非线性自回归神经网络,粗糙集方法和每月替换。在非线性自回归网络中发现了很高的估计精度(均方根误差(RMSE)约为0:03 m3 = m3),这是因为其基于回归的动态网络允许通过离散时间估计进行反馈连接。在粗糙集过程中,同样高的精度(0.05 m3 = m3 RMSE)说明了土壤水分在时间上持久性的重要作用,并具有解决不同土壤水分条件的能力。

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