Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition

The hydro-climatology of Colombia exhibits strong natural variability at a broad range of time scales including: inter-decadal, decadal, inter-annual, annual, intra-annual, intra-seasonal, and diurnal. Diverse applied sectors rely on quantitative predictions of river discharges for operational purpo...

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Main Authors: A. M. Carmona, G. Poveda
Format: Article
Language:English
Published: Copernicus Publications 2015-04-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/366/172/2015/piahs-366-172-2015.pdf
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spelling doaj-26e05663480341f88a06e840633b06552020-11-24T23:48:00ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-04-0136617217210.5194/piahs-366-172-2015Prediction of mean monthly river discharges in Colombia through Empirical Mode DecompositionA. M. Carmona0G. Poveda1Department of Geosciences and Environment, Universidad Nacional de Colombia at Medellín, Carrera 80 No 65-223 &ndash; Núcleo Robledo, Medellín, ColombiaDepartment of Geosciences and Environment, Universidad Nacional de Colombia at Medellín, Carrera 80 No 65-223 &ndash; Núcleo Robledo, Medellín, ColombiaThe hydro-climatology of Colombia exhibits strong natural variability at a broad range of time scales including: inter-decadal, decadal, inter-annual, annual, intra-annual, intra-seasonal, and diurnal. Diverse applied sectors rely on quantitative predictions of river discharges for operational purposes including hydropower generation, agriculture, human health, fluvial navigation, territorial planning and management, risk preparedness and mitigation, among others. Various methodologies have been used to predict monthly mean river discharges that are based on "Predictive Analytics", an area of statistical analysis that studies the extraction of information from historical data to infer future trends and patterns. Our study couples the Empirical Mode Decomposition (EMD) with traditional methods, e.g. Autoregressive Model of Order 1 (AR1) and Neural Networks (NN), to predict mean monthly river discharges in Colombia, South America. <br><br> The EMD allows us to decompose the historical time series of river discharges into a finite number of intrinsic mode functions (IMF) that capture the different oscillatory modes of different frequencies associated with the inherent time scales coexisting simultaneously in the signal (Huang et al. 1998, Huang and Wu 2008, Rao and Hsu, 2008). Our predictive method states that it is easier and simpler to predict each IMF at a time and then add them up together to obtain the predicted river discharge for a certain month, than predicting the full signal. This method is applied to 10 series of monthly mean river discharges in Colombia, using calibration periods of more than 25 years, and validation periods of about 12 years. Predictions are performed for time horizons spanning from 1 to 12 months. Our results show that predictions obtained through the traditional methods improve when the EMD is used as a previous step, since errors decrease by up to 13% when the AR1 model is used, and by up to 18% when using Neural Networks is combined with the EMD.https://www.proc-iahs.net/366/172/2015/piahs-366-172-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. M. Carmona
G. Poveda
spellingShingle A. M. Carmona
G. Poveda
Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
Proceedings of the International Association of Hydrological Sciences
author_facet A. M. Carmona
G. Poveda
author_sort A. M. Carmona
title Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
title_short Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
title_full Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
title_fullStr Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
title_full_unstemmed Prediction of mean monthly river discharges in Colombia through Empirical Mode Decomposition
title_sort prediction of mean monthly river discharges in colombia through empirical mode decomposition
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2015-04-01
description The hydro-climatology of Colombia exhibits strong natural variability at a broad range of time scales including: inter-decadal, decadal, inter-annual, annual, intra-annual, intra-seasonal, and diurnal. Diverse applied sectors rely on quantitative predictions of river discharges for operational purposes including hydropower generation, agriculture, human health, fluvial navigation, territorial planning and management, risk preparedness and mitigation, among others. Various methodologies have been used to predict monthly mean river discharges that are based on "Predictive Analytics", an area of statistical analysis that studies the extraction of information from historical data to infer future trends and patterns. Our study couples the Empirical Mode Decomposition (EMD) with traditional methods, e.g. Autoregressive Model of Order 1 (AR1) and Neural Networks (NN), to predict mean monthly river discharges in Colombia, South America. <br><br> The EMD allows us to decompose the historical time series of river discharges into a finite number of intrinsic mode functions (IMF) that capture the different oscillatory modes of different frequencies associated with the inherent time scales coexisting simultaneously in the signal (Huang et al. 1998, Huang and Wu 2008, Rao and Hsu, 2008). Our predictive method states that it is easier and simpler to predict each IMF at a time and then add them up together to obtain the predicted river discharge for a certain month, than predicting the full signal. This method is applied to 10 series of monthly mean river discharges in Colombia, using calibration periods of more than 25 years, and validation periods of about 12 years. Predictions are performed for time horizons spanning from 1 to 12 months. Our results show that predictions obtained through the traditional methods improve when the EMD is used as a previous step, since errors decrease by up to 13% when the AR1 model is used, and by up to 18% when using Neural Networks is combined with the EMD.
url https://www.proc-iahs.net/366/172/2015/piahs-366-172-2015.pdf
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