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Applicability of multilayer feed-forward neural networks to model the onset of river breakup

机译:多层前馈神经网络在河道破裂模型中的适用性

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摘要

Predicting the onset of breakup is an essential component of any ice jam flood forecasting system, yet it presents a difficult challenge due to the complex nature of the relationship between meteorological conditions, streamflow hydraulics and ice mechanics. For this research, data extracted from historical hydrometric and meteorological records were used to develop and assess a three-layer feed-forward artificial neural network (ANN) model for predicting the onset of breakup, using the Hay River in northern Canada as the demonstration site. The calibration results illustrate the potential of the ANN model for successful forecasting of the onset of river ice breakup, i.e. the first transverse cracking of the ice cover. However, rigorous validation also indicates that the accuracy of such ANN models can be optimistically overestimated by their performance during the calibration phase. The possible reasons for this poor predictive capability of the ANN model are also discussed. Despite this caveat, the proposed model shows improved performance as compared to the more conventional multiple linear regression (MLR) techniques typically applied to this problem.
机译:预测破裂的发生是任何冰堵洪水预报系统的重要组成部分,但是由于气象条件,水流水力和冰力学之间关系的复杂性,它提出了一个艰巨的挑战。对于这项研究,以加拿大北部的海河为示范点,使用从历史水文和气象记录中提取的数据来开发和评估三层前馈人工神经网络(ANN)模型,以预测破裂的发生。 。校准结果说明了ANN模型在成功预测河冰破裂,即首次冰盖横向破裂方面的潜力。但是,严格的验证也表明,此类ANN模型的准确性可能会因其在校准阶段的性能而被乐观地高估。还讨论了ANN模型预测能力差的可能原因。尽管有这些警告,但与通常应用于此问题的更常规的多元线性回归(MLR)技术相比,所提出的模型显示出更高的性能。

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