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Comparative Analysis of Training Methods and Different Data for the Rainfall-Runoff Predication Using Artificial Neural Networks

机译:人工神经网络用于降雨径流预报的训练方法和不同数据的比较分析

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Hydrology and climatic monthly data's influence on training of Artificial Neural Networks (ANNs) for monthly rain fall prediction is investigated. For improved computed performances, efficiencies of the Conjugate Gradient (CG) and Levenberg-Marquardt (L-M) training algorithms are compared. The rain fall-run off influence is studied for a watershed in Northern Iran, representing a continuous rain fall-run off with stream flow regime occurring. The used data in ANN was hydrometric and climatic monthly data with 31 years duration from 1969 to 2000. For the mentioned model 27 year's data were used for its development but for the validation/testing of the model 4 years data was applied. Based on the results, the L-M algorithm is more efficient than the CG algorithm, so it is used to train six ANNs models for rain fall-runoff prediction at time step t+1 from time step t input. The used network in this study was MLP with B.P. (back propagation) algorithm. Model 1 uses enabled rain fall data as input dimension with use tree station, Model 2 uses enabled rain fall and average temperature, Model 3 uses enabled rain fall, average temperature and stream flow at time step t-1 and Model 4 uses enabled rain fall and stream flow at time step (t, t-1, t-2), Model 5 uses enabled rain fall and stream flow at time step (t, t-1, t-2.t-3) Model 6 uses enabled rain fall, average temperature and stream flow at time step (t-1, t-2). Validation stage Root Mean Square Error (RMSE), Root Mean Absolute Error (RMAE) and Correlation Coefficient (R) measures are: 0.07, 6×10~(-4), 0.99 (Model 1); 0.1, 9×10~(-4), 0.99 (Model 2); 0.01, 9×10~(-5), 1 (Model 3); 0.005, 6×10~(-5), 1 (Model 4); 0.001, 0.7×10~(-5), 1 (Model 5); 0.001, 6×10~(-5), 1 (Model 6) and, respectively. The influence of rain fall and stream flow at time step (t, t-1, t-2) on improved Model 4 performance is discussed.
机译:研究了水文和气候月度数据对人工神经网络训练对降雨预测的影响。为了提高计算性能,比较了共轭梯度(CG)和Levenberg-Marquardt(L-M)训练算法的效率。研究了伊朗北部一个流域的降雨径流的影响,这代表了连续的降雨径流和水流状态的发生。 ANN中使用的数据是1969年至2000年的31年的水文和气候月度数据。对于上述模型,使用了27年的数据进行开发,但使用了4年的模型进行验证/测试。基于结果,L-M算法比CG算法更有效,因此它被用来训练六个ANN模型以从时间步t输入开始的时间步t + 1进行降雨径流预测。本研究中使用的网络是具有B.P. (反向传播)算法。模型1使用启用的降雨数据作为使用树站的输入维,模型2使用启用的降雨和平均温度,模型3使用启用的降雨,时间步t-1的平均温度和水流,模型4使用启用的降雨。和时间步长(t,t-1,t-2)的水流量,模型5使用时间步长(t,t-1,t-2.t-3)的模型6使用时间步长的雨水下降,平均温度和时间步长(t-1,t-2)的水流。验证阶段的均方根误差(RMSE),均方根绝对误差(RMAE)和相关系数(R)度量为:0.07、6×10〜(-4),0.99(模型1); 0.1,9×10〜(-4),0.99(模型2); 0.01,9×10〜(-5),1(模型3); 0.005,6×10〜(-5),1(模型4); 0.001,0.7×10〜(-5),1(型号5);分别为0.001、6×10〜(-5),1(模型6)和。讨论了降雨和时间步长(t,t-1,t-2)的水流对改进Model 4性能的影响。

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