Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated

Streamflow fluctuates as a result of different atmospheric, hydrologic, and morphologic mechanisms governing a river watershed. Variability of meteorological variables such as rainfall, temperature, wind, sea level pressure, humidity, and heating, as well as large scale climate indices like the Arct...

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Main Author: Rasouli, Kabir
Format: Thesis
Language:English
Published: University of British Columbia 2010
Subjects:
Online Access:http://hdl.handle.net/2429/27090
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spelling ftunivbritcolcir:oai:circle.library.ubc.ca:2429/27090 2023-05-15T15:03:38+02:00 Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated Rasouli, Kabir 2010 http://hdl.handle.net/2429/27090 eng eng University of British Columbia Attribution-NonCommercial-NoDerivs 3.0 Unported http://creativecommons.org/licenses/by-nc-nd/3.0/ CC-BY-NC-ND Text Thesis/Dissertation 2010 ftunivbritcolcir 2019-10-15T17:58:49Z Streamflow fluctuates as a result of different atmospheric, hydrologic, and morphologic mechanisms governing a river watershed. Variability of meteorological variables such as rainfall, temperature, wind, sea level pressure, humidity, and heating, as well as large scale climate indices like the Arctic Oscillation, Pacific/North American Pattern, North Atlantic Oscillation, and El Niño-Southern Oscillation play a role on the availability of water in a given basin. In this study, outputs of the NOAA Global Forecasting System (GFS) model, climate fluctuations, and observed data from meteohydrologic stations are used to forecast daily streamflows. Three machine learning methods are used for this purpose: support vector regression (SVR), Gaussian process (GP), and Bayesian neural network (BNN) models, and the results are compared with the multiple linear regression (MLR) model. Lead-time for forecasting varies from 1 to 7 days. This study has been applied to a small coastal watershed in British Columbia, Canada. Model comparisons show the BNN model tends to slightly outperform the GP and SVR models and all three models perform better than the MLR model. The results show that as predictors the observed data and the GFS model outputs are most effective at shorter lead-times while observed data and climate indices are most effective at longer lead-times. When the leadtime increases, climate indices such as the Arctic Oscillation, the North Atlantic Oscillation, and the Niño 3.4 which measures the central equatorial Pacific sea surface temperature (SST) anomalies, become more important in influencing the streamflow variability. The Nash-Sutcliffe forecast skill scores based on the naive methods of climatology, persistence, and a combination of them for all data and the Peirce Skill Score (PSS) and Extreme Dependency Score (EDS) for the streamflow rare events are evaluated for the BNN model. For rare events the skill scores are better when the predictors are the GFS outputs plus locally observed data compared to cases when only observed data or any combination of observed and climate indices are chosen as the predictors. Science, Faculty of Earth, Ocean and Atmospheric Sciences, Department of Graduate Thesis Arctic North Atlantic North Atlantic oscillation University of British Columbia: cIRcle - UBC's Information Repository Arctic British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada Nash ENVELOPE(-62.350,-62.350,-74.233,-74.233) Pacific Sutcliffe ENVELOPE(-81.383,-81.383,50.683,50.683)
institution Open Polar
collection University of British Columbia: cIRcle - UBC's Information Repository
op_collection_id ftunivbritcolcir
language English
description Streamflow fluctuates as a result of different atmospheric, hydrologic, and morphologic mechanisms governing a river watershed. Variability of meteorological variables such as rainfall, temperature, wind, sea level pressure, humidity, and heating, as well as large scale climate indices like the Arctic Oscillation, Pacific/North American Pattern, North Atlantic Oscillation, and El Niño-Southern Oscillation play a role on the availability of water in a given basin. In this study, outputs of the NOAA Global Forecasting System (GFS) model, climate fluctuations, and observed data from meteohydrologic stations are used to forecast daily streamflows. Three machine learning methods are used for this purpose: support vector regression (SVR), Gaussian process (GP), and Bayesian neural network (BNN) models, and the results are compared with the multiple linear regression (MLR) model. Lead-time for forecasting varies from 1 to 7 days. This study has been applied to a small coastal watershed in British Columbia, Canada. Model comparisons show the BNN model tends to slightly outperform the GP and SVR models and all three models perform better than the MLR model. The results show that as predictors the observed data and the GFS model outputs are most effective at shorter lead-times while observed data and climate indices are most effective at longer lead-times. When the leadtime increases, climate indices such as the Arctic Oscillation, the North Atlantic Oscillation, and the Niño 3.4 which measures the central equatorial Pacific sea surface temperature (SST) anomalies, become more important in influencing the streamflow variability. The Nash-Sutcliffe forecast skill scores based on the naive methods of climatology, persistence, and a combination of them for all data and the Peirce Skill Score (PSS) and Extreme Dependency Score (EDS) for the streamflow rare events are evaluated for the BNN model. For rare events the skill scores are better when the predictors are the GFS outputs plus locally observed data compared to cases when only observed data or any combination of observed and climate indices are chosen as the predictors. Science, Faculty of Earth, Ocean and Atmospheric Sciences, Department of Graduate
format Thesis
author Rasouli, Kabir
spellingShingle Rasouli, Kabir
Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
author_facet Rasouli, Kabir
author_sort Rasouli, Kabir
title Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
title_short Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
title_full Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
title_fullStr Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
title_full_unstemmed Short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
title_sort short lead-time streamflow forecasting by machine learning methods, with climate variability incorporated
publisher University of British Columbia
publishDate 2010
url http://hdl.handle.net/2429/27090
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
ENVELOPE(-62.350,-62.350,-74.233,-74.233)
ENVELOPE(-81.383,-81.383,50.683,50.683)
geographic Arctic
British Columbia
Canada
Nash
Pacific
Sutcliffe
geographic_facet Arctic
British Columbia
Canada
Nash
Pacific
Sutcliffe
genre Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
North Atlantic
North Atlantic oscillation
op_rights Attribution-NonCommercial-NoDerivs 3.0 Unported
http://creativecommons.org/licenses/by-nc-nd/3.0/
op_rightsnorm CC-BY-NC-ND
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