Multiple model combination methods for annual maximum water level prediction during river ice breakup

Abstract The Athabasca River is the largest unregulated river in Alberta, Canada, with ice jams frequently occurring in the vicinity of Fort McMurray. Modelling tools are desired to forecast ice‐related flood events. Multiple model combination methods can often obtain better predictive performances...

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Published in:Hydrological Processes
Main Authors: Sun, Wei, Trevor, Bernard
Other Authors: Alberta Environment and Parks
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2018
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.11429
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spelling crwiley:10.1002/hyp.11429 2024-09-15T17:55:11+00:00 Multiple model combination methods for annual maximum water level prediction during river ice breakup Sun, Wei Trevor, Bernard Alberta Environment and Parks 2018 http://dx.doi.org/10.1002/hyp.11429 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.11429 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.11429 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 32, issue 3, page 421-435 ISSN 0885-6087 1099-1085 journal-article 2018 crwiley https://doi.org/10.1002/hyp.11429 2024-09-05T05:07:32Z Abstract The Athabasca River is the largest unregulated river in Alberta, Canada, with ice jams frequently occurring in the vicinity of Fort McMurray. Modelling tools are desired to forecast ice‐related flood events. Multiple model combination methods can often obtain better predictive performances than any member models due to possible variance reduction of forecast errors or correction of biases. However, few applications of this method to river ice forecasting are reported. Thus, a framework of multiple model combination methods for maximum breakup water level (MBWL) Prediction during river ice breakup is proposed. Within the framework, the member models describe the relations between the MBWL (predicted variable) and their corresponding indicators (predictor variables); the combining models link the relations between the predicted MBWL by each member model and the observed MBWL. Especially, adaptive neuro‐fuzzy inference systems, artificial neural networks, and multiple linear regression are not only employed as member models but also as combining models. Simple average methods (SAM) are selected as the basic combining model due to simple calculations. In the SAM, an equal weight (1/n) is assigned to n member models. The historical breakup data of the Athabasca River at Fort McMurray for the past 36 years (1980 to 2015) are collected to facilitate the comparison of models. These models are examined using the leave‐one‐out cross validation and the holdout validation methods. A SAM, which is the average output from three optimal member models, is selected as the best model as it has the optimal validation performance (lowest average squared errors). In terms of lowest average squared errors, the SAM improves upon the optimal artificial neural networks, adaptive neuro‐fuzzy inference systems, and multiple linear regression member models by 21.95%, 30.97%, and 24.03%, respectively. This result sheds light on the effectiveness of combining different forecasting models when a scarce river ice data set is ... Article in Journal/Newspaper Athabasca River Fort McMurray Wiley Online Library Hydrological Processes 32 3 421 435
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The Athabasca River is the largest unregulated river in Alberta, Canada, with ice jams frequently occurring in the vicinity of Fort McMurray. Modelling tools are desired to forecast ice‐related flood events. Multiple model combination methods can often obtain better predictive performances than any member models due to possible variance reduction of forecast errors or correction of biases. However, few applications of this method to river ice forecasting are reported. Thus, a framework of multiple model combination methods for maximum breakup water level (MBWL) Prediction during river ice breakup is proposed. Within the framework, the member models describe the relations between the MBWL (predicted variable) and their corresponding indicators (predictor variables); the combining models link the relations between the predicted MBWL by each member model and the observed MBWL. Especially, adaptive neuro‐fuzzy inference systems, artificial neural networks, and multiple linear regression are not only employed as member models but also as combining models. Simple average methods (SAM) are selected as the basic combining model due to simple calculations. In the SAM, an equal weight (1/n) is assigned to n member models. The historical breakup data of the Athabasca River at Fort McMurray for the past 36 years (1980 to 2015) are collected to facilitate the comparison of models. These models are examined using the leave‐one‐out cross validation and the holdout validation methods. A SAM, which is the average output from three optimal member models, is selected as the best model as it has the optimal validation performance (lowest average squared errors). In terms of lowest average squared errors, the SAM improves upon the optimal artificial neural networks, adaptive neuro‐fuzzy inference systems, and multiple linear regression member models by 21.95%, 30.97%, and 24.03%, respectively. This result sheds light on the effectiveness of combining different forecasting models when a scarce river ice data set is ...
author2 Alberta Environment and Parks
format Article in Journal/Newspaper
author Sun, Wei
Trevor, Bernard
spellingShingle Sun, Wei
Trevor, Bernard
Multiple model combination methods for annual maximum water level prediction during river ice breakup
author_facet Sun, Wei
Trevor, Bernard
author_sort Sun, Wei
title Multiple model combination methods for annual maximum water level prediction during river ice breakup
title_short Multiple model combination methods for annual maximum water level prediction during river ice breakup
title_full Multiple model combination methods for annual maximum water level prediction during river ice breakup
title_fullStr Multiple model combination methods for annual maximum water level prediction during river ice breakup
title_full_unstemmed Multiple model combination methods for annual maximum water level prediction during river ice breakup
title_sort multiple model combination methods for annual maximum water level prediction during river ice breakup
publisher Wiley
publishDate 2018
url http://dx.doi.org/10.1002/hyp.11429
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.11429
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.11429
genre Athabasca River
Fort McMurray
genre_facet Athabasca River
Fort McMurray
op_source Hydrological Processes
volume 32, issue 3, page 421-435
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.11429
container_title Hydrological Processes
container_volume 32
container_issue 3
container_start_page 421
op_container_end_page 435
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