Widespread flooding dynamics under climate change: characterising floods using grid-based hydrological modelling and regional climate projections

• Published in: Hydrology and earth system sciences 2024-06, Vol.28 (12), p.2635-2650
• Main Authors: Griffin, Adam, Kay, Alison L, Sayers, Paul, Bell, Victoria, Stewart, Elizabeth, Carr, Sam
• Format: Article
• Language: English
• Subjects: Analysis; Climate change; Climate effects; Climate models; Climatic changes; Flood management; Floods; Hydrologic models; Hydrology; Precipitation; Regional climate models; Regional climates; Risk management; River flow; Stream flow; Temperature; United Kingdom
• ISSN: 1607-7938; 1027-5606; 1607-7938
• DOI: 10.5194/hess-28-2635-2024

An event-based approach has been used to explore the potential effects of climate change on the spatial and temporal coherence of widespread flood events in Great Britain. Time series of daily mean river flow were generated using a gridded national-scale hydrological model (Grid-to-Grid) driven by a 12-member ensemble of regional climate projections from UK Climate Projections 2018 (UKCP18), for 30-year baseline (1980–2010) and future (2050–2080) time slices. From these, sets of widespread extreme events were extracted. The question of what defines a “widespread flood event” is discussed; here it was defined as an event exceeding an at-site 99.5th percentile (equivalent to 2 d per year) simultaneously over an area of at least 20 km2, with a maximum duration of 14 d. This resulted in a set of 14 400 widespread events: approximately 20 events per year, per ensemble member, per time slice. Overall, results have shown that events are more temporally concentrated in winter in the future time slice compared to the baseline. Distributions of event area were similar in both time slices, but the distribution of at-site return periods showed some heavier tails in the future time slice. Such information could be useful for adaptation planning and risk management for floods under climate change, but the potential future changes have to be interpreted in the context of some differences in event characteristics between the baseline climate-projection-driven model runs and an observation-driven model run. While the focus here is Great Britain, the methods and analyses described could be applied to other regions with hydrological models and climate projections of appropriate resolution.