Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming

Abstract The hydrological characteristics of a river, including the magnitude and timing of high and low flows, are important determinants of its ecological functioning. Climate change will alter these characteristics, triggering ecological changes in river ecosystems. This study assesses risks of e...

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Autores principales: J. R. Thompson, S. N. Gosling, J. Zaherpour, C. L. R. Laizé
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Lenguaje:EN
Publicado: American Geophysical Union (AGU) 2021
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Acceso en línea:https://doaj.org/article/ba92f6cbdd05435ab75e13cbcc663c3e
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spelling oai:doaj.org-article:ba92f6cbdd05435ab75e13cbcc663c3e2021-11-23T18:30:30ZIncreasing Risk of Ecological Change to Major Rivers of the World With Global Warming2328-427710.1029/2021EF002048https://doaj.org/article/ba92f6cbdd05435ab75e13cbcc663c3e2021-11-01T00:00:00Zhttps://doi.org/10.1029/2021EF002048https://doaj.org/toc/2328-4277Abstract The hydrological characteristics of a river, including the magnitude and timing of high and low flows, are important determinants of its ecological functioning. Climate change will alter these characteristics, triggering ecological changes in river ecosystems. This study assesses risks of ecological change in 321 major river basins across the globe due to global warming relative to pre‐industrial conditions of 1.0, 1.5, 2.0 and 3.0°C. Risks associated with climate‐driven changes to high and low flows, relative to baseline (1980–2010; 0.6°C warming), are investigated using simulations from nine global hydrological models forced with climate projections from five global climate models, resulting in an ensemble of 14,445 baseline‐scenario members for each warming scenario (9 × 5 × 321). At the global‐scale, the likelihood of high risks of significant ecological change in both high and low flows increase with global warming: across all basins there is a medium‐high risk of change in high (low) flows in 21.4% (22.4%) of ensemble members for 1.0°C warming, increasing to 61.5% (63.2%) for 3.0°C. Risks are particularly pronounced for low flows at 3.0°C for many rivers in South America, southern Africa, Australia, southern Europe and central and eastern USA. Results suggest that boreal regions are least likely to see significant ecological change due to modified river flows but this may be partly the result of the exclusion of processes such as permafrost dynamics from most global hydrological models. The study highlights the ecological fragility and spatial heterogeneity of the risks that unmitigated climate change poses to global river ecosystems.J. R. ThompsonS. N. GoslingJ. ZaherpourC. L. R. LaizéAmerican Geophysical Union (AGU)articleclimate changeenvironmental flowsriver ecologyglobal hydrologyhigh flowslow flowsEnvironmental sciencesGE1-350EcologyQH540-549.5ENEarth's Future, Vol 9, Iss 11, Pp n/a-n/a (2021)
institution DOAJ
collection DOAJ
language EN
topic climate change
environmental flows
river ecology
global hydrology
high flows
low flows
Environmental sciences
GE1-350
Ecology
QH540-549.5
spellingShingle climate change
environmental flows
river ecology
global hydrology
high flows
low flows
Environmental sciences
GE1-350
Ecology
QH540-549.5
J. R. Thompson
S. N. Gosling
J. Zaherpour
C. L. R. Laizé
Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
description Abstract The hydrological characteristics of a river, including the magnitude and timing of high and low flows, are important determinants of its ecological functioning. Climate change will alter these characteristics, triggering ecological changes in river ecosystems. This study assesses risks of ecological change in 321 major river basins across the globe due to global warming relative to pre‐industrial conditions of 1.0, 1.5, 2.0 and 3.0°C. Risks associated with climate‐driven changes to high and low flows, relative to baseline (1980–2010; 0.6°C warming), are investigated using simulations from nine global hydrological models forced with climate projections from five global climate models, resulting in an ensemble of 14,445 baseline‐scenario members for each warming scenario (9 × 5 × 321). At the global‐scale, the likelihood of high risks of significant ecological change in both high and low flows increase with global warming: across all basins there is a medium‐high risk of change in high (low) flows in 21.4% (22.4%) of ensemble members for 1.0°C warming, increasing to 61.5% (63.2%) for 3.0°C. Risks are particularly pronounced for low flows at 3.0°C for many rivers in South America, southern Africa, Australia, southern Europe and central and eastern USA. Results suggest that boreal regions are least likely to see significant ecological change due to modified river flows but this may be partly the result of the exclusion of processes such as permafrost dynamics from most global hydrological models. The study highlights the ecological fragility and spatial heterogeneity of the risks that unmitigated climate change poses to global river ecosystems.
format article
author J. R. Thompson
S. N. Gosling
J. Zaherpour
C. L. R. Laizé
author_facet J. R. Thompson
S. N. Gosling
J. Zaherpour
C. L. R. Laizé
author_sort J. R. Thompson
title Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
title_short Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
title_full Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
title_fullStr Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
title_full_unstemmed Increasing Risk of Ecological Change to Major Rivers of the World With Global Warming
title_sort increasing risk of ecological change to major rivers of the world with global warming
publisher American Geophysical Union (AGU)
publishDate 2021
url https://doaj.org/article/ba92f6cbdd05435ab75e13cbcc663c3e
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