Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches

Abstract Under future climate scenarios, possible changes of drought patterns pose new challenges for water resources management. For quantifying and qualifying drought characteristics in the UK, the drought severity indices of six catchments are investigated and modelled by two stochastic methods:...

Full description

Bibliographic Details
Published in:Hydrological Processes
Main Authors: Chun, Kwok Pan, Wheater, Howard, Onof, Christian
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.9259
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9259
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9259
id crwiley:10.1002/hyp.9259
record_format openpolar
spelling crwiley:10.1002/hyp.9259 2024-06-23T07:55:11+00:00 Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches Chun, Kwok Pan Wheater, Howard Onof, Christian 2012 http://dx.doi.org/10.1002/hyp.9259 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9259 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9259 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 27, issue 11, page 1600-1614 ISSN 0885-6087 1099-1085 journal-article 2012 crwiley https://doi.org/10.1002/hyp.9259 2024-06-13T04:24:18Z Abstract Under future climate scenarios, possible changes of drought patterns pose new challenges for water resources management. For quantifying and qualifying drought characteristics in the UK, the drought severity indices of six catchments are investigated and modelled by two stochastic methods: autoregressive integrated moving average (ARIMA) models and the generalized linear model (GLM) approach. From the ARIMA models, autocorrelation structures are first identified for the drought index series, and the unexplained variance of the series is used to establish empirical relationships between drought and climate variables. Based on the ARIMA results, mean sea level pressure and possibly the North Atlantic Oscillation index are found to be significant climate variables for seasonal drought forecasting. Using the GLM approach, occurrences and amounts of rainfall are simulated with conditioning on climate variables. From the GLM‐simulated rainfall for the 1980s and 2080s, the probabilistic characteristics of the drought severity are derived and assessed. Results indicate that the drought pattern in the 2080s is less certain than for the 1961–1990 period, based on the Shannon entropy, but that droughts are expected to be more clustered and intermittent. The 10th and 50th quantiles of drought are likely higher in the 2080s scenarios, but there is no evidence showing the changes in the 90th quantile extreme droughts. Copyright © 2012 John Wiley & Sons, Ltd. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Hydrological Processes 27 11 1600 1614
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Under future climate scenarios, possible changes of drought patterns pose new challenges for water resources management. For quantifying and qualifying drought characteristics in the UK, the drought severity indices of six catchments are investigated and modelled by two stochastic methods: autoregressive integrated moving average (ARIMA) models and the generalized linear model (GLM) approach. From the ARIMA models, autocorrelation structures are first identified for the drought index series, and the unexplained variance of the series is used to establish empirical relationships between drought and climate variables. Based on the ARIMA results, mean sea level pressure and possibly the North Atlantic Oscillation index are found to be significant climate variables for seasonal drought forecasting. Using the GLM approach, occurrences and amounts of rainfall are simulated with conditioning on climate variables. From the GLM‐simulated rainfall for the 1980s and 2080s, the probabilistic characteristics of the drought severity are derived and assessed. Results indicate that the drought pattern in the 2080s is less certain than for the 1961–1990 period, based on the Shannon entropy, but that droughts are expected to be more clustered and intermittent. The 10th and 50th quantiles of drought are likely higher in the 2080s scenarios, but there is no evidence showing the changes in the 90th quantile extreme droughts. Copyright © 2012 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Chun, Kwok Pan
Wheater, Howard
Onof, Christian
spellingShingle Chun, Kwok Pan
Wheater, Howard
Onof, Christian
Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
author_facet Chun, Kwok Pan
Wheater, Howard
Onof, Christian
author_sort Chun, Kwok Pan
title Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
title_short Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
title_full Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
title_fullStr Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
title_full_unstemmed Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches
title_sort prediction of the impact of climate change on drought: an evaluation of six uk catchments using two stochastic approaches
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1002/hyp.9259
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9259
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9259
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Hydrological Processes
volume 27, issue 11, page 1600-1614
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.9259
container_title Hydrological Processes
container_volume 27
container_issue 11
container_start_page 1600
op_container_end_page 1614
_version_ 1802647654310608896