Attribution of long-term changes in peak river flows in Great Britain

We investigate the evidence for changes in the magnitude of peak river flows in Great Britain. We focus on a set of 117 near-natural “benchmark” catchments to detect trends not driven by land use and other human impacts, and aim to attribute trends in peak river flows to some climate indices such as...

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Main Authors: Brady, Aoibheann, Faraway, Julian, Prosdocimi, Ilaria
Format: Text
Language:unknown
Published: Taylor & Francis 2019
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.8319848.v1
https://tandf.figshare.com/articles/Attribution_of_long-term_changes_in_peak_river_flows_in_Great_Britain/8319848/1
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spelling ftdatacite:10.6084/m9.figshare.8319848.v1 2023-05-15T17:33:20+02:00 Attribution of long-term changes in peak river flows in Great Britain Brady, Aoibheann Faraway, Julian Prosdocimi, Ilaria 2019 https://dx.doi.org/10.6084/m9.figshare.8319848.v1 https://tandf.figshare.com/articles/Attribution_of_long-term_changes_in_peak_river_flows_in_Great_Britain/8319848/1 unknown Taylor & Francis https://dx.doi.org/10.1080/02626667.2019.1628964 https://dx.doi.org/10.6084/m9.figshare.8319848 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Space Science Ecology FOS Biological sciences Sociology FOS Sociology Cancer Inorganic Chemistry FOS Chemical sciences Plant Biology Text article-journal Journal contribution ScholarlyArticle 2019 ftdatacite https://doi.org/10.6084/m9.figshare.8319848.v1 https://doi.org/10.1080/02626667.2019.1628964 https://doi.org/10.6084/m9.figshare.8319848 2021-11-05T12:55:41Z We investigate the evidence for changes in the magnitude of peak river flows in Great Britain. We focus on a set of 117 near-natural “benchmark” catchments to detect trends not driven by land use and other human impacts, and aim to attribute trends in peak river flows to some climate indices such as the North Atlantic Oscillation (NAO) and the East Atlantic (EA) index. We propose modelling all stations together in a Bayesian multilevel framework to be better able to detect any signal that is present in the data by pooling information across several stations. This approach leads to the detection of a clear countrywide time trend. Additionally, in a univariate approach, both the EA and NAO indices appear to have a considerable association with peak river flows. When a multivariate approach is taken to unmask the collinearity between climate indices and time, the association between NAO and peak flows disappears, while the association with EA remains clear. This demonstrates the usefulness of a multivariate and multilevel approach when it comes to accurately attributing trends in peak river flows. Text North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Space Science
Ecology
FOS Biological sciences
Sociology
FOS Sociology
Cancer
Inorganic Chemistry
FOS Chemical sciences
Plant Biology
spellingShingle Space Science
Ecology
FOS Biological sciences
Sociology
FOS Sociology
Cancer
Inorganic Chemistry
FOS Chemical sciences
Plant Biology
Brady, Aoibheann
Faraway, Julian
Prosdocimi, Ilaria
Attribution of long-term changes in peak river flows in Great Britain
topic_facet Space Science
Ecology
FOS Biological sciences
Sociology
FOS Sociology
Cancer
Inorganic Chemistry
FOS Chemical sciences
Plant Biology
description We investigate the evidence for changes in the magnitude of peak river flows in Great Britain. We focus on a set of 117 near-natural “benchmark” catchments to detect trends not driven by land use and other human impacts, and aim to attribute trends in peak river flows to some climate indices such as the North Atlantic Oscillation (NAO) and the East Atlantic (EA) index. We propose modelling all stations together in a Bayesian multilevel framework to be better able to detect any signal that is present in the data by pooling information across several stations. This approach leads to the detection of a clear countrywide time trend. Additionally, in a univariate approach, both the EA and NAO indices appear to have a considerable association with peak river flows. When a multivariate approach is taken to unmask the collinearity between climate indices and time, the association between NAO and peak flows disappears, while the association with EA remains clear. This demonstrates the usefulness of a multivariate and multilevel approach when it comes to accurately attributing trends in peak river flows.
format Text
author Brady, Aoibheann
Faraway, Julian
Prosdocimi, Ilaria
author_facet Brady, Aoibheann
Faraway, Julian
Prosdocimi, Ilaria
author_sort Brady, Aoibheann
title Attribution of long-term changes in peak river flows in Great Britain
title_short Attribution of long-term changes in peak river flows in Great Britain
title_full Attribution of long-term changes in peak river flows in Great Britain
title_fullStr Attribution of long-term changes in peak river flows in Great Britain
title_full_unstemmed Attribution of long-term changes in peak river flows in Great Britain
title_sort attribution of long-term changes in peak river flows in great britain
publisher Taylor & Francis
publishDate 2019
url https://dx.doi.org/10.6084/m9.figshare.8319848.v1
https://tandf.figshare.com/articles/Attribution_of_long-term_changes_in_peak_river_flows_in_Great_Britain/8319848/1
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://dx.doi.org/10.1080/02626667.2019.1628964
https://dx.doi.org/10.6084/m9.figshare.8319848
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.8319848.v1
https://doi.org/10.1080/02626667.2019.1628964
https://doi.org/10.6084/m9.figshare.8319848
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