2015
DOI: 10.1016/j.jhydrol.2014.11.053
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Real-time error correction method combined with combination flood forecasting technique for improving the accuracy of flood forecasting

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Cited by 60 publications
(23 citation statements)
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“…We notice that the upper Yangtze River' tributaries have notoriously complex hydro-geological characteristics. Plenty of studies were devoted to developing reliable and accurate short-term (less than 24-h ahead) flood forecast models for the Yangtze River due to the extremely non-linear relationship between rainfall and runoff over this basin during storm events [50,51]. Besides, a small improvement in the reliability and accuracy of short-term flood forecasts could be critical and beneficial to flood prevention as well as the dynamic management of the TGR.…”
Section: Evaluation Indicatorsmentioning
confidence: 99%
“…We notice that the upper Yangtze River' tributaries have notoriously complex hydro-geological characteristics. Plenty of studies were devoted to developing reliable and accurate short-term (less than 24-h ahead) flood forecast models for the Yangtze River due to the extremely non-linear relationship between rainfall and runoff over this basin during storm events [50,51]. Besides, a small improvement in the reliability and accuracy of short-term flood forecasts could be critical and beneficial to flood prevention as well as the dynamic management of the TGR.…”
Section: Evaluation Indicatorsmentioning
confidence: 99%
“…Therefore, we coupled these criterions to examine the descriptive strength of PD S and hence choose the most reliable marginal distribution. RMSE and AIC are defined by the following equations [37,38]…”
Section: Selection Of Marginal Distributionmentioning
confidence: 99%
“…The output/ error assimilation methods treat a streamflow forecast as a pure model output and update it by adding errors calculated with another independent procedure or model. Such procedures/models could either be nonlinear, such as artificial neural networks (ANNs; Anctil et al 2003), or linear, such as autoregressive-moving-average models (Broersen 2007, Chen et al 2015. Output/error assimilation of streamflow is relatively simple to implement, as there is no feedback to the original RR model from the manipulation of model outputs.…”
Section: Hydrological Da Targetsmentioning
confidence: 99%