Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North

The Red River of the North is vulnerable to floods, which have caused significant damage and economic loss to inhabitants. A better capability in flood-event prediction is essential to decision-makers for planning flood-loss-reduction strategies. Over the last decades, classical statistical methods...

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Main Authors: Vida Atashi, Hamed Taheri Gorji, Seyed Mojtaba Shahabi, Ramtin Kardan, Yeo Howe Lim
Format: Article
Language:English
Published: MDPI AG 2022-06-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/14/12/1971
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author Vida Atashi
Hamed Taheri Gorji
Seyed Mojtaba Shahabi
Ramtin Kardan
Yeo Howe Lim
author_facet Vida Atashi
Hamed Taheri Gorji
Seyed Mojtaba Shahabi
Ramtin Kardan
Yeo Howe Lim
author_sort Vida Atashi
collection DOAJ
description The Red River of the North is vulnerable to floods, which have caused significant damage and economic loss to inhabitants. A better capability in flood-event prediction is essential to decision-makers for planning flood-loss-reduction strategies. Over the last decades, classical statistical methods and Machine Learning (ML) algorithms have greatly contributed to the growth of data-driven forecasting systems that provide cost-effective solutions and improved performance in simulating the complex physical processes of floods using mathematical expressions. To make improvements to flood prediction for the Red River of the North, this paper presents effective approaches that make use of a classical statistical method, a classical ML algorithm, and a state-of-the-art Deep Learning method. Respectively, the methods are seasonal autoregressive integrated moving average (SARIMA), Random Forest (RF), and Long Short-Term Memory (LSTM). We used hourly level records from three U.S. Geological Survey (USGS), at Pembina, Drayton, and Grand Forks stations with twelve years of data (2007–2019), to evaluate the water level at six hours, twelve hours, one day, three days, and one week in advance. Pembina, at the downstream location, has a water level gauge but not a flow-gauging station, unlike the others. The floodwater-level-prediction results show that the LSTM method outperforms the SARIMA and RF methods. For the one-week-ahead prediction, the RMSE values for Pembina, Drayton, and Grand Forks are 0.190, 0.151, and 0.107, respectively. These results demonstrate the high precision of the Deep Learning algorithm as a reliable choice for flood-water-level prediction.
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spelling doaj.art-176a9154342447c791f98d8c3f3bd4e72023-11-23T19:30:37ZengMDPI AGWater2073-44412022-06-011412197110.3390/w14121971Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the NorthVida Atashi0Hamed Taheri Gorji1Seyed Mojtaba Shahabi2Ramtin Kardan3Yeo Howe Lim4Department of Civil Engineering, University of North Dakota, Grand Forks, ND 58202, USADepartment of Biomedical Engineering, University of North Dakota, Grand Forks, ND 58202, USASchool of Electrical Engineering & Computer Science, University of North Dakota, Grand Forks, ND 58202, USADepartment of Mechanical Engineering, University of North Dakota, Grand Forks, ND 58202, USADepartment of Civil Engineering, University of North Dakota, Grand Forks, ND 58202, USAThe Red River of the North is vulnerable to floods, which have caused significant damage and economic loss to inhabitants. A better capability in flood-event prediction is essential to decision-makers for planning flood-loss-reduction strategies. Over the last decades, classical statistical methods and Machine Learning (ML) algorithms have greatly contributed to the growth of data-driven forecasting systems that provide cost-effective solutions and improved performance in simulating the complex physical processes of floods using mathematical expressions. To make improvements to flood prediction for the Red River of the North, this paper presents effective approaches that make use of a classical statistical method, a classical ML algorithm, and a state-of-the-art Deep Learning method. Respectively, the methods are seasonal autoregressive integrated moving average (SARIMA), Random Forest (RF), and Long Short-Term Memory (LSTM). We used hourly level records from three U.S. Geological Survey (USGS), at Pembina, Drayton, and Grand Forks stations with twelve years of data (2007–2019), to evaluate the water level at six hours, twelve hours, one day, three days, and one week in advance. Pembina, at the downstream location, has a water level gauge but not a flow-gauging station, unlike the others. The floodwater-level-prediction results show that the LSTM method outperforms the SARIMA and RF methods. For the one-week-ahead prediction, the RMSE values for Pembina, Drayton, and Grand Forks are 0.190, 0.151, and 0.107, respectively. These results demonstrate the high precision of the Deep Learning algorithm as a reliable choice for flood-water-level prediction.https://www.mdpi.com/2073-4441/14/12/1971flood predictionwater levelRed RiverSARIMARFLSTM
spellingShingle Vida Atashi
Hamed Taheri Gorji
Seyed Mojtaba Shahabi
Ramtin Kardan
Yeo Howe Lim
Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
Water
flood prediction
water level
Red River
SARIMA
RF
LSTM
title Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
title_full Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
title_fullStr Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
title_full_unstemmed Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
title_short Water Level Forecasting Using Deep Learning Time-Series Analysis: A Case Study of Red River of the North
title_sort water level forecasting using deep learning time series analysis a case study of red river of the north
topic flood prediction
water level
Red River
SARIMA
RF
LSTM
url https://www.mdpi.com/2073-4441/14/12/1971
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