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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American Geophysical Union (AGU)
2021
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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) |
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climate change environmental flows river ecology global hydrology high flows low flows Environmental sciences GE1-350 Ecology QH540-549.5 |
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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 |
work_keys_str_mv |
AT jrthompson increasingriskofecologicalchangetomajorriversoftheworldwithglobalwarming AT sngosling increasingriskofecologicalchangetomajorriversoftheworldwithglobalwarming AT jzaherpour increasingriskofecologicalchangetomajorriversoftheworldwithglobalwarming AT clrlaize increasingriskofecologicalchangetomajorriversoftheworldwithglobalwarming |
_version_ |
1718416177968971776 |