Professor SIMON GOSLING SIMON.GOSLING@NOTTINGHAM.AC.UK
PROFESSOR OF CLIMATE RISKS AND ENVIRONMENTAL MODELLING
A comparison of changes in river runoff from multiple global and catchment-scale hydrological models under global warming scenarios of 1°C, 2°C and 3°C
Gosling, Simon; Zaherpour, Jamal; Mount, Nick J.; Hattermann, Fred; Dankers, Rutger; Arheimer, Berit; Breuer, Lutz; Ding, Jie; Haddeland, Ingjerd; Kumar, Rohini; Kundu, Dipangkar; Liu, Junguo; van Griensven, Ann; Veldkamp, Ted; Vetter, Tobias; Wang, Xiaoyan; Zhang, Xinxin
Authors
Jamal Zaherpour
Professor NICK MOUNT nick.mount@nottingham.ac.uk
Chief Executive UoN Online
Fred Hattermann
Rutger Dankers
Berit Arheimer
Lutz Breuer
Jie Ding
Ingjerd Haddeland
Rohini Kumar
Dipangkar Kundu
Junguo Liu
Ann van Griensven
Ted Veldkamp
Tobias Vetter
Xiaoyan Wang
Xinxin Zhang
Abstract
We present one of the first climate change impact assessments on river runoff that utilises an ensemble of global hydrological models (Glob-HMs) and an ensemble of catchment-scale hydrological models (Cat-HMs), across multiple catchments: the upper Amazon, Darling, Ganges, Lena, upper Mississippi, upper Niger, Rhine and Tagus. Relative changes in simulated mean annual runoff (MAR) and four indicators of high and low extreme flows are compared between the two ensembles. The ensemble median values of changes in runoff with three different scenarios of global-mean warming (1°C, 2°C and 3°C above pre-industrial levels) are generally similar between the two ensembles, although the ensemble spread is often larger for the Glob-HM ensemble. In addition the ensemble spread is normally larger than the difference between the two ensemble medians. Whilst we find compelling evidence for projected runoff changes for the Rhine (decrease), Tagus (decrease) and Lena (increase) with global warming, the sign and magnitude of change for the other catchments is unclear. Our model results highlight that for these three catchments in particular, global climate change mitigation, which limits global-mean temperature rise to below 2°C above pre-industrial levels, could avoid some of the hydrological hazards that could be seen with higher magnitudes of global warming.
Citation
Gosling, S., Zaherpour, J., Mount, N. J., Hattermann, F., Dankers, R., Arheimer, B., Breuer, L., Ding, J., Haddeland, I., Kumar, R., Kundu, D., Liu, J., van Griensven, A., Veldkamp, T., Vetter, T., Wang, X., & Zhang, X. (in press). A comparison of changes in river runoff from multiple global and catchment-scale hydrological models under global warming scenarios of 1°C, 2°C and 3°C. Climatic Change, https://doi.org/10.1007/s10584-016-1773-3
Journal Article Type | Article |
---|---|
Acceptance Date | Jul 25, 2016 |
Online Publication Date | Nov 9, 2016 |
Deposit Date | Jul 29, 2016 |
Publicly Available Date | Nov 9, 2016 |
Journal | Climatic Change |
Print ISSN | 0165-0009 |
Electronic ISSN | 1573-1480 |
Publisher | Springer Verlag |
Peer Reviewed | Peer Reviewed |
DOI | https://doi.org/10.1007/s10584-016-1773-3 |
Keywords | Global warming; hydrology; UNFCCC 2°C target; climate change; extremes; runoff |
Public URL | https://nottingham-repository.worktribe.com/output/829433 |
Publisher URL | http://link.springer.com/article/10.1007%2Fs10584-016-1773-3 |
Contract Date | Jul 29, 2016 |
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Copyright Statement
Copyright information regarding this work can be found at the following address: http://creativecommons.org/licenses/by/4.0
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