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Suspended sediment flux modelling in a transboundary Himalayan river basin

机译:跨界喜马拉雅河流域悬浮泥沙通量模拟

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Artificial neural network (ANN) models have been developed for simulation of daily suspended sediment flux in the Subansiri River basin, which is a transboundary eastern Himalayan basin and the biggest sub-basin of the Brahmaputra River in India. Modelling was conducted on two datasets: (1) daily discharge and suspended sediment concentration data of 15 years (1993-2007) and (2) daily data of climate (rainfall, temperature) and snow cover area along with discharge and suspended sediment concentration for six years (2001, 2003-2007). The performance of ANN models has been compared with conventional sediment rating curves (SRC) and multiple linear regression models (MLR) having similar input data. ANN models were found to be considerably better than the SRC and MLR models. This paper concludes by providing discussion about how the different type of input data, length of input data and lagging of input data affects the accuracy of sediment flux estimation in a large Himalayan River basin and also provides guidance on the types of tasks for which different types of input data may be preferable.
机译:已经开发出了人工神经网络(ANN)模型,用于模拟Subansiri流域的每日悬浮泥沙通量,Subansiri流域是喜马拉雅东部的跨界盆地,是印度Brahmaputra河的最大子流域。对两个数据集进行了建模:(1)15年(1993-2007年)的每日排放量和悬浮泥沙浓度数据,以及(2)气候(降雨,温度)和积雪面积的每日数据以及排放量和悬浮泥沙浓度。六年(2001年,2003-2007年)。已将ANN模型的性能与具有相似输入数据的常规沉积物额定曲线(SRC)和多个线性回归模型(MLR)进行了比较。发现ANN模型比SRC和MLR模型要好得多。本文最后通过讨论不同类型的输入数据,输入数据的长度和输入数据的滞后如何影响喜马拉雅大流域的泥沙通量估算的准确性,并为不同类型任务的类型提供指导输入数据的数量可能更可取。

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