Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations

Abstract The present study applies different time‐series models for forecasting daily and monthly snow water equivalent (SWE) data in Ontario, Canada, during 1987–2011. For daily time series, which showed a significant negative trend, four categories of the autoregressive moving‐average (ARMA) and A...

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Published in:Hydrological Processes
Main Authors: Sarhadi, Ali, Kelly, Richard, Modarres, Reza
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.10184
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spelling crwiley:10.1002/hyp.10184 2024-06-02T08:11:29+00:00 Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations Sarhadi, Ali Kelly, Richard Modarres, Reza 2014 http://dx.doi.org/10.1002/hyp.10184 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10184 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10184 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 28, issue 16, page 4640-4653 ISSN 0885-6087 1099-1085 journal-article 2014 crwiley https://doi.org/10.1002/hyp.10184 2024-05-03T11:13:14Z Abstract The present study applies different time‐series models for forecasting daily and monthly snow water equivalent (SWE) data in Ontario, Canada, during 1987–2011. For daily time series, which showed a significant negative trend, four categories of the autoregressive moving‐average (ARMA) and ARMA model with exogenous variables (ARMAX) were applied. The North Atlantic Oscillation, Southern Oscillation Index and Pacific/North American Pattern, as large‐scale atmospheric anomalies, as well as temperature time series are considered as exogenous variables for ARMAX models. According to the multicriteria performance evaluation, a time‐trend ARMAX model demonstrated the best performance for modelling and forecasting daily SWE. Two models, seasonal autoregressive integrated moving average (SARIMA) and SARIMA with exogenous variables (SARIMAX), were also fitted to the monthly SWE time series. The results revealed that the SARIMAX model showed a better performance than the SARIMA model according to multicriteria evaluation. The three nonparametric tests, Wilcoxon, Levene and Kolmogorov–Smirnov for forecasting evaluation demonstrated that the selected time‐series models had enough reliability for short‐term SWE forecasting in Ontario. The results of this study also demonstrate the importance of incorporating both trend and appropriate exogenous variables for SWE time‐series modelling and forecasting. Copyright © 2014 John Wiley & Sons, Ltd. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Canada Pacific Sarima ENVELOPE(29.040,29.040,69.037,69.037) Hydrological Processes 28 16 4640 4653
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The present study applies different time‐series models for forecasting daily and monthly snow water equivalent (SWE) data in Ontario, Canada, during 1987–2011. For daily time series, which showed a significant negative trend, four categories of the autoregressive moving‐average (ARMA) and ARMA model with exogenous variables (ARMAX) were applied. The North Atlantic Oscillation, Southern Oscillation Index and Pacific/North American Pattern, as large‐scale atmospheric anomalies, as well as temperature time series are considered as exogenous variables for ARMAX models. According to the multicriteria performance evaluation, a time‐trend ARMAX model demonstrated the best performance for modelling and forecasting daily SWE. Two models, seasonal autoregressive integrated moving average (SARIMA) and SARIMA with exogenous variables (SARIMAX), were also fitted to the monthly SWE time series. The results revealed that the SARIMAX model showed a better performance than the SARIMA model according to multicriteria evaluation. The three nonparametric tests, Wilcoxon, Levene and Kolmogorov–Smirnov for forecasting evaluation demonstrated that the selected time‐series models had enough reliability for short‐term SWE forecasting in Ontario. The results of this study also demonstrate the importance of incorporating both trend and appropriate exogenous variables for SWE time‐series modelling and forecasting. Copyright © 2014 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Sarhadi, Ali
Kelly, Richard
Modarres, Reza
spellingShingle Sarhadi, Ali
Kelly, Richard
Modarres, Reza
Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
author_facet Sarhadi, Ali
Kelly, Richard
Modarres, Reza
author_sort Sarhadi, Ali
title Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
title_short Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
title_full Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
title_fullStr Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
title_full_unstemmed Snow water equivalent time‐series forecasting in Ontario, Canada, in link to large atmospheric circulations
title_sort snow water equivalent time‐series forecasting in ontario, canada, in link to large atmospheric circulations
publisher Wiley
publishDate 2014
url http://dx.doi.org/10.1002/hyp.10184
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10184
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10184
long_lat ENVELOPE(29.040,29.040,69.037,69.037)
geographic Canada
Pacific
Sarima
geographic_facet Canada
Pacific
Sarima
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Hydrological Processes
volume 28, issue 16, page 4640-4653
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.10184
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