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Coupling soil moisture and precipitation observations for predicting hourly runoff at small catchment scale

机译:耦合土壤水分和降水观测以预测小集水区小时径流量

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摘要

The importance of soil moisture is recognized in rainfall-runoff processes. This study quantitatively investigates the use of soil moisture measured at 10, 20, and 40cm soil depths along with rainfall in predicting runoff. For this purpose, two small sub-catchments of Tiber River Basin, in Italy, were instrumented during periods of October 2002-March 2003 and January-April 2004. Colorso Basin is about 13km2 and Niccone basin 137km2. Rainfall plus soil moisture at 10, 20, and 40cm formed the input vector while the discharge was the target output in the model of generalized regression neural network (GRNN). The model for each basin was calibrated and tested using October 2002-March 2003 data. The calibrated and tested GRNN was then employed to predict runoff for each basin for the period of January-April 2004. The model performance was found to be satisfactory with determination coefficient, R2, equal to 0.87 and Nash-Sutcliffe efficiency, NS, equal to 0.86 in the validation phase for both catchments. The investigation of effects of soil moisture on runoff prediction revealed that the addition of soil moisture data, along with rainfall, tremendously improves the performance of the model. The sensitivity analysis indicated that the use of soil moisture data at different depths allows to preserve the memory of the system thus having a similar effect of employing the past values of rainfall, but with improved GRNN performance.
机译:在降雨径流过程中已经认识到土壤水分的重要性。这项研究定量研究了在10、20和40cm土层深度测量的土壤湿度以及降雨在预测径流中的用途。为此,在2002年10月至2003年3月和2004年1月至2004年4月期间,对意大利的台伯河流域的两个小流域进行了监测。Colorso流域约13 km2,Niccone流域137 km2。广义回归神经网络(GRNN)模型中,降雨,土壤水分在10、20和40cm处形成输入向量,而流量则是目标输出。使用2002年10月至2003年3月的数据对每个盆地的模型进行了校准和测试。然后,使用经过校准和测试的GRNN来预测2004年1月至4月期间每个流域的径流量。模型性能令人满意,确定系数R2等于0.87,纳什-苏特克利夫效率NS等于两个流域的验证阶段为0.86。对土壤水分对径流预测的影响的调查表明,增加土壤水分数据以及降雨可以极大地改善模型的性能。敏感性分析表明,使用不同深度的土壤湿度数据可以保留系统的内存,因此具有使用过去降雨值的类似效果,但GRNN性能有所提高。

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