2017
DOI: 10.1016/j.jhydrol.2017.03.003
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Multi-scale quantitative precipitation forecasting using nonlinear and nonstationary teleconnection signals and artificial neural network models

Abstract: Global sea surface temperature (SST) anomalies are observed to have a significant effect on terrestrial precipitation patterns throughout the United States. SST variations have been correlated with terrestrial precipitation via ocean-atmospheric interactions known as climate teleconnections. This study demonstrates how the scale effect could affect the forecasting accuracy with or without the inclusion of those newly discovered unknown teleconnection signals between Adirondack precipitation and SST anomaly in … Show more

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Cited by 15 publications
(19 citation statements)
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“…In order to verify the accuracy of the multivariations LSTM model more over the traditional single-variation LSTM model, the single-variation LSTM (1) [15] model (using the runoff volume of the previous time period to predict the runoff volume of the next moment) and the multivariations LSTM (2) [29], model (using the rainfall of the previous time period to predict the runoff volume of the next moment) were selected as comparison models. Moreover, the single-variation EEMD-LSTM (1) [16] model and the EEMD-LSTM multivariations model (the EEMD-LSTM (2) model, which is a multivariations LSTM model with the main variables reconstructed by EEMD decomposition, and the EEMD-LSTM (3) model, which has the model input variables added to the remaining meteorological factors as secondary variables for runoff prediction) were selected as comparison models to verify the effectiveness of the EEMD method. The input and output settings of each model are shown in Table 4.…”
Section: Suitability Analysis Of the Eemd-lstm Multivariations Modelmentioning
confidence: 99%
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“…In order to verify the accuracy of the multivariations LSTM model more over the traditional single-variation LSTM model, the single-variation LSTM (1) [15] model (using the runoff volume of the previous time period to predict the runoff volume of the next moment) and the multivariations LSTM (2) [29], model (using the rainfall of the previous time period to predict the runoff volume of the next moment) were selected as comparison models. Moreover, the single-variation EEMD-LSTM (1) [16] model and the EEMD-LSTM multivariations model (the EEMD-LSTM (2) model, which is a multivariations LSTM model with the main variables reconstructed by EEMD decomposition, and the EEMD-LSTM (3) model, which has the model input variables added to the remaining meteorological factors as secondary variables for runoff prediction) were selected as comparison models to verify the effectiveness of the EEMD method. The input and output settings of each model are shown in Table 4.…”
Section: Suitability Analysis Of the Eemd-lstm Multivariations Modelmentioning
confidence: 99%
“…LSTM (1) Historical runoff None runoff runoff LSTM (2) Historical rainfall, runoff None rainfall runoff EEMD-LSTM (1) Historical runoff EEMD IMF 1 -IMF n , R IMF 1 -IMF n , R EEMD-LSTM (2) Historical rainfall, runoff EEMD, K-means K 1 -K d runoff EEMD-LSTM (3) Historical meteorological factors, runoff EEMD, K-means K 1 -K d , meteorological factors runoff Table 5. Comparison of simulation results of various models.…”
Section: Required Documents Preprocessing Input Features Output Labelsmentioning
confidence: 99%
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“…With the development of artificial intelligence prediction model, it has been widely used in precipitation forecasting research in recent years. Chang et al [11] established a wavelet analysis combined with artificial neural network (ANN) model to predict 30-year non-linear and unsteady precipitation signals in a certain area. The results show that this method has higher forecasting precision than the traditional method.…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, runoff and sediment systems are highly complex, and they are influenced by various factors, such that the time series or multi-temporal component series of runoff and sediment discharge may be nonstationary (Chang et al, 2017). Nevertheless, previous studies on the time series of hydrological variables have usually assumed that the time series are stationary, and they have thereby constructed steady-state models.…”
Section: Introductionmentioning
confidence: 99%