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Assessing the performance of eight real-time updating models and procedures for the Brosna River

机译:评估Brosna河的八个实时更新模型和程序的性能

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The flow forecasting performance of eight updating models, incorporated inthe Galway River Flow Modelling and Forecasting System (GFMFS), was assessedusing daily data (rainfall, evaporation and discharge) of the Irish Brosnacatchment (1207 km2), considering their one to six days lead-time dischargeforecasts. The Perfect Forecast of Input over the Forecast Lead-time scenariowas adopted, where required, in place of actual rainfall forecasts. The eightupdating models were: (i) the standard linear Auto-Regressive (AR) model,applied to the forecast errors (residuals) of a simulation (non-updating)rainfall-runoff model; (ii) the Neural Network Updating (NNU) model, alsousing such residuals as input; (iii) the Linear Transfer Function (LTF)model, applied to the simulated and the recently observed discharges; (iv)the Non-linear Auto-Regressive eXogenous-Input Model (NARXM), also a neuralnetwork-type structure, but having wide options of using recently observedvalues of one or more of the three data series, together with non-updatedsimulated outflows, as inputs; (v) the Parametric Simple Linear Model (PSLM),of LTF-type, using recent rainfall and observed discharge data; (vi) theParametric Linear perturbation Model (PLPM), also of LTF-type, using recentrainfall and observed discharge data, (vii) n-AR, an AR model applied to theobserved discharge series only, as a na?ve updating model; and (viii)n-NARXM, a naive form of the NARXM, using only the observed discharge data,excluding exogenous inputs. The five GFMFS simulation (non-updating) modelsused were the non-parametric and parametric forms of the Simple Linear Modeland of the Linear Perturbation Model, the Linearly-Varying Gain Factor Model,the Artificial Neural Network Model, and the conceptual Soil MoistureAccounting and Routing (SMAR) model. As the SMAR model performance was foundto be the best among these models, in terms of the Nash-Sutcliffe R2 value,both in calibration and in verification, the simulated outflows of this modelonly were selected for the subsequent exercise of producing updated dischargeforecasts. All the eight forms of updating models for producing lead-timedischarge forecasts were found to be capable of producing relatively goodlead-1 (1-day ahead) forecasts, with R2 values almost 90% or above. However,for higher lead time forecasts, only three updating models, viz., NARXM, LTF,and NNU, were found to be suitable, with lead-6 values of R2 about 90% orhigher. Graphical comparisons were made of the lead-time forecasts for thetwo largest floods, one in the calibration period and the other in theverification period.
机译:使用爱尔兰Brosnatchatatchation(1207 km 2 )的每日数据(雨量,蒸发量和流量)评估了纳入戈尔韦河流量建模和预报系统(GFMFS)中的八个更新模型的流量预报性能,考虑其一到六天的提前期放电预测。在需要时采用了在预测提前期上进行的输入的完美预测,代替了实际的降雨预测。八个更新模型是:(i)标准线性自回归(AR)模型,应用于模拟(非更新)降雨-径流模型的预测误差(残差); (ii)神经网络更新(NNU)模型,也使用这些残差作为输入; (iii)线性传递函数(LTF)模型,适用于模拟放电和最近观察到的放电; (iv)非线性自回归异质输入模型(NARXM),也是一种神经网络类型的结构,但是具有使用三个数据系列中一个或多个的最近观测值以及未更新的模拟流出的多种选择,作为输入; (v)LTF型的参数简单线性模型(PSLM),使用最近的降雨和观测到的流量数据; (vi)使用最近降雨和观测到的排放数据的LTF型参数线性摄动模型(vii)n-AR,仅适用于观测排放序列的AR模型,作为简单的更新模型; (viii)n-NARXM,NARXM的原始形式,仅使用观察到的排放数据,不包括外来输入。使用的五个GFMFS模拟(非更新)模型是简单线性模型和线性摄动模型,线性变化增益因子模型,人工神经网络模型以及概念性土壤水分会计和路由的非参数形式和参数形式。 (SMAR)模型。由于SMAR模型的性能在这些模型中是最好的,因此就Nash-Sutcliffe R 2 值而言,无论是在标定还是在验证中,仅选择此模型用于后续的生产更新的排放预测。发现用于生成提前期放电预测的所有八种更新模​​型都能够生成相对良好的Lead-1预测(提前1天),其值为 R 2 几乎90%或以上。但是,对于更高的提前期预测,仅找到三种更新模型,即NARXM,LTF和NNU,并且其Lead-6值为 R 2 约90%或更高。对两次最大洪水的提前期预测进行了图形比较,一次是在校准期,另一次是在验证期。

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