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Assessing artificial neural networks coupled with waveletanalysis for multi-layer soil moisture dynamics pr

机译:评估人工神经网络与小波分析相结合的多层土壤水分动力学

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Soil moisture simulation and prediction in semi-arid regions are important for agricultural production, soil conservation andclimate change. However, considerable heterogeneity in the spatial distribution of soil moisture, and poor ability of distributedhydrological models to estimate it, severely impact the use of soil moisture models in research and practical applications. Inthis study, a newly-developed technique of coupled (WA-ANN) wavelet analysis (WA) and artificial neural network (ANN)was applied for a multi-layer soil moisture simulation in the Pailugou catchment of the Qilian Mountains, Gansu Province,China. Datasets included seven meteorological factors: air and land surface temperatures, relative humidity, global radiation,atmospheric pressure, wind speed, precipitation, and soil water content at 20, 40, 60, 80, 120 and 160 cm. To investigate theeffectiveness of WA-ANN, ANN was applied by itself to conduct a comparison. Three main findings of this study were: (1)ANN and WA-ANN provided a statistically reliable and robust prediction of soil moisture in both the root zone and deepestsoil layer studied (NSE 〉0.85, NSE means Nash-Sutcliffe Efficiency coefficient); (2) when input meteorological factors weretransformed using maximum signal to noise ratio (SNR) and one-dimensional auto de-noising algorithm (heursure) in WA,the coupling technique improved the performance of ANN especially for soil moisture at 160 cm depth; (3) the results ofmulti-layer soil moisture prediction indicated that there may be different sources of water at different soil layers, and this canbe used as an indicator of the maximum impact depth of meteorological factors on the soil water content at this study site. Weconclude that our results show that appropriate simulation methodology can provide optimal simulation with a minimumdistortion of the raw-time series; the new method used here is applicable to soil sciences and management applications.
机译:半干旱地区的土壤水分模拟和预测对农业生产,土壤保持和气候变化具有重要意义。但是,土壤水分空间分布的异质性很大,而分布式水文模型估计能力差,严重影响了土壤水分模型在研究和实际应用中的使用。在这项研究中,将新开发的(WA-ANN)小波分析(WA)和人工神经网络(ANN)耦合技术应用于甘肃省祁连山牌楼沟流域的多层土壤水分模拟中。数据集包括七个气象因子:空气和陆地表面温度,相对湿度,全球辐射,大气压,风速,降水以及20、40、60、80、120和160 cm处的土壤水分。为了研究WA-ANN的有效性,将ANN本身进行了比较。这项研究的三个主要发现是:(1)ANN和WA-ANN提供了统计上可靠且鲁棒的预测研究根区和最深土壤层的水分(NSE> 0.85,NSE表示纳什-苏特克利夫效率系数); (2)在WA中采用最大信噪比(SNR)和一维自动降噪算法(heursure)对输入气象因子进行转换时,耦合技术提高了人工神经网络的性能,特别是对于160cm深度的土壤水分。 (3)多层土壤含水量预测结果表明,不同土壤层可能存在不同的水源,可作为该研究地点气象因子对土壤含水量最大影响深度的指标。我们认为结果表明适当的仿真方法可以在原始时间序列失真最小的情况下提供最佳仿真。这里使用的新方法适用于土壤科学和管理应用。

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