4.7 Article

Climate change effects on indicators of high and low river flow across Great Britain

Journal

ADVANCES IN WATER RESOURCES
Volume 151, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.advwatres.2021.103909

Keywords

Climate change; Hydrological impacts; Rainfall-runoff; UKCP18; Flood; Drought

Funding

  1. Natural Environment Research Council [NE/S016457/2]
  2. NERC [NE/S016457/2] Funding Source: UKRI

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Research suggests that in the future, there is generally a trend of decreasing low flows and increasing high flows in the UK. There is significant regional variation in these changes, with the south/east regions showing a more pronounced decrease in low flows. Significant variation within regions, likely related to catchment properties, has also been observed.
Changes in river flows, especially extreme high and low flows, could be a particularly important impact of climate change in terms of the hazard to people and the environment. Here, a national-scale grid-based hydrological model is applied, with ensembles of global and regional climate projections from UK Climate Projections 2018, to investigate the potential future changes in both floods and droughts in a consistent way across the whole of Great Britain (gauged and ungauged locations). Using hydrological model outputs for the climate projection ensembles, a clustering technique is applied to highlight ?typical? sets of changes in individual indicators of floods or droughts, but also to look at concurrent changes in pairs of flood and drought indicators. The results for regions across the country generally indicate decreases in low flows combined with increases in high flows up to the end of the 21st century. There is significant variation in results for different regions, with those to the south/east tending to show greater decreases in low flows and a greater range of uncertainty in the projections for high flows. A grid-based cluster analysis also shows potentially important variation within regions, likely related to catchment properties. The potential future changes in derived climate hazards, such as the frequency or severity of floods and droughts, is a key piece of information required for adaptation planning, and the consideration of potential concurrent changes in a range of related hazards/risks, rather than viewing each in isolation, could be vital to avoid maladaptation.

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