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Eco-hydrological estimation of event-based runoff coefficient using artificial intelligence models in Kasilian watershed, Iran

机译:基于事件的径流系数在伊朗kasilian流域的智能模型生态水文估算

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摘要

In this research, estimation of the Runoff Coefficient (RC) is carried out depending on land cover. Initially, RC modeling was performed using 54 hourly rainfall and corresponding runoff data during the period 1987-2010 in the Kasilian watershed. Artificial Neural Network (ANN), Adaptive Neuro-Fuzzy Inference System (ANFIS) and Support Vector Regression (SVR) models and effective factors including rainfall intensity, phi index (the average loss), five-day previous rainfall and Normalized Difference Vegetation Index (NDVI) were used to estimate RC. The results showed that the ANN model was more efficient than the other two models and had Mean Bias Error (MBE), Coefficient of Determination (R-2), Nash-Sutcliffe Efficiency (NSE) and Normalized Root Mean Square Error (NRMSE) equal to 0.08, 0.85, 0.84 and 0.37, respectively for the training phase and 0.12, 0.76, 0.74 and 0.47 for the test phase. In general, it is suggested that RC plays a major role in hydrological mechanisms and flooding. Thus, optimal estimation of RC can be helpful in better management of soil and water conservation and erosion and sediment management in this area.
机译:在该研究中,根据陆地覆盖来进行径流系数(RC)的估计。最初,RC建模在Kasilian流域的1987-2010期间使用54小时降雨和相应的径流数据进行。人工神经网络(ANN),自适应神经模糊推理系统(ANFIS)和支持向量回归(SVR)模型和有效因素,包括降雨强度,PHI指数(平均损失),五天之前的降雨和归一化差异植被指数( NDVI)用于估计RC。结果表明,ANN模型比其他两个模型更有效,并且具有平均偏差误差(MBE),确定系数(R-2),NASH-SUTCLIFFE效率(NSE)和归一化的根均线误差(NRMSE)等于分别为训练相和0.08,0.85,0.84和0.37,测试阶段为0.12,0.76,0.74和0.47。一般来说,建议RC在水文机制和洪水中发挥着重要作用。因此,RC的最佳估计可能有助于在该地区的水土保持和水保存和腐蚀和沉积物管理方面有所帮助。

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