Revisiting hydro-ecological impacts of climate change on a restored floodplain wetland via hydrological/hydraulic modelling and the UK Climate Projections 2018 scenarios
Thompson, Julian R.; Clilverd, Hannah M. ORCID: https://orcid.org/0000-0001-6771-3302; Zheng, Jiaxuan; Iravani, Honeyeh; Sayer, Carl D.; Heppell, Catherine M.; Axmacher, Jan C.. 2023 Revisiting hydro-ecological impacts of climate change on a restored floodplain wetland via hydrological/hydraulic modelling and the UK Climate Projections 2018 scenarios. Wetlands, 43 (6), 71. 44, pp. 10.1007/s13157-023-01708-0
Before downloading, please read NORA policies.Preview |
Text
N536032JA.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (6MB) | Preview |
Abstract/Summary
The hydro-ecological impacts of 40 UK Climate Projections 2018 scenarios on a restored lowland England river floodplain are assessed using a MIKE SHE / MIKE 11 model. Annual precipitation declines for 60% of scenarios (range: -26%–21%, with small, <5%, declines for the central probability level). Potential evapotranspiration increases for all probability levels except the most extreme, very unlikely, 10% level (range: -4%–43%, central probability 9%–20%) Mean, peak and low river discharges are reduced for all but the extreme 90% probability level. Reduced frequency of bankfull discharge dominates (at least halved for the central probability level). Floodplain inundation declines for over 97% of 320 scenario-events. Winter water table levels still intercept the surface, while mean and summer low levels are reduced. Declines in mean summer floodplain water table levels for the central probability level (0.22 m and 0.28 m for the 2050s and 2080s, respectively) are twice as large as those in the more dynamic riparian area. Declines reach 0.39 m for some 10% probability level scenarios. Simulated hydrological changes differ subtly from a previous assessment using earlier UK climate projections. A soil aeration stress index demonstrates that, under baseline conditions, prolonged high winter floodplain water tables drive long periods of low root-zone oxygen, in turn favouring vegetation communities adapted to waterlogged conditions. Climate change reduces aeration stress and the extent of appropriate conditions for these plant communities in favour of communities less tolerant of wet conditions.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | 10.1007/s13157-023-01708-0 |
UKCEH and CEH Sections/Science Areas: | Atmospheric Chemistry and Effects (Science Area 2017-) |
ISSN: | 0277-5212 |
Additional Information. Not used in RCUK Gateway to Research.: | Open Access paper - full text available via Official URL link. |
Additional Keywords: | climate change, floodplain, MIKE SHE, UKCP18, aeration stress |
NORA Subject Terms: | Ecology and Environment Hydrology Atmospheric Sciences Data and Information |
Related URLs: | |
Date made live: | 09 Nov 2023 12:43 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/536032 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year