Modelling the impact of future climate change on streamflow and water quality in Wales, UK
Research output: Contribution to journal › Article › peer-review
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In: Hydrological Sciences Journal, Vol. 67, No. 6, 25.04.2022, p. 939-962.
Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Modelling the impact of future climate change on streamflow and water quality in Wales, UK
AU - Dallison, Richard
AU - Williams, Prysor
AU - Harris, Ian
AU - Patil, Sopan
PY - 2022/4/25
Y1 - 2022/4/25
N2 - Climate change is likely to have a major impact on future hydrological regimes, impacting numerous sectors reliant on surface waters. We use the Soil and Water Assessment Tool (SWAT) to model future (2021-2080) streamflow and water quality variables (nitrogen, phosphorus, suspended sediment, and dissolved oxygen), in five catchments in Wales, under a worst-case scenario of future greenhouse gas concentrations (RCP8.5). Results show a decline in annual average flows (-4% to -13%) but larger changes seasonally (spring, up to 41% increase; autumn, up to 52% reduction). The magnitude and frequency of high flow events increases in spring (magnitude: Sen’s slope range 0.165-0.589, p <0.01), with more low flows in autumn (Sen’s slope range 0.064-0.090, p <0.01). Water quality declines, with higher nitrogen, phosphorus, and sediment concentrations and lower dissolved oxygen levels. The findings have economic and environmental implications for abstractors, as water resources could become more unreliable, seasonal, and polluted.
AB - Climate change is likely to have a major impact on future hydrological regimes, impacting numerous sectors reliant on surface waters. We use the Soil and Water Assessment Tool (SWAT) to model future (2021-2080) streamflow and water quality variables (nitrogen, phosphorus, suspended sediment, and dissolved oxygen), in five catchments in Wales, under a worst-case scenario of future greenhouse gas concentrations (RCP8.5). Results show a decline in annual average flows (-4% to -13%) but larger changes seasonally (spring, up to 41% increase; autumn, up to 52% reduction). The magnitude and frequency of high flow events increases in spring (magnitude: Sen’s slope range 0.165-0.589, p <0.01), with more low flows in autumn (Sen’s slope range 0.064-0.090, p <0.01). Water quality declines, with higher nitrogen, phosphorus, and sediment concentrations and lower dissolved oxygen levels. The findings have economic and environmental implications for abstractors, as water resources could become more unreliable, seasonal, and polluted.
KW - UKCP18
KW - hydrological modelling
KW - particle swarm optimization
KW - trend analysis
KW - water resource management
KW - water supply
U2 - 10.1080/02626667.2022.2044045
DO - 10.1080/02626667.2022.2044045
M3 - Article
VL - 67
SP - 939
EP - 962
JO - Hydrological Sciences Journal
JF - Hydrological Sciences Journal
SN - 0262-6667
IS - 6
ER -