Abstract

Study regionNorthern Ireland (NI), and sub-catchments in the Republic of Ireland that drain to NI rivers, Study focusInformation on the potential future impacts of climate change on river flows is necessary for adaptation planning. There have been many such studies for Great Britain, but fewer for NI. Here, a grid-based hydrological model is configured for NI, and used to investigate changes in seasonal mean, extreme high and extreme low flows. New Hydrological InsightsWhen driven by observed climate data, the model shows good performance for a wide range of catchments, particularly where artificial influences are limited. When driven by ensemble data from the UKCP18 Regional (12 km) projections, model performance for the baseline period (1981–2010) is similar to that using observed data, especially when using a simple precipitation bias-correction. Model projections for a future time-slice (2051–2080) generally suggest decreases in spring–autumn mean flows, especially in summer (median −44%), but possible increases in winter mean flows (median 9%), with some variation between ensemble members, particularly in winter when some show large increases to the west. Consistent with this are large projected reductions in 10-year return period low flows everywhere (median −45%), and large increases in 10-year return period high flows for some locations and ensemble members (median 16%). Future applications could include expanding the range of climate data applied.

Highlights

  • Information on the potential future impacts of climate change on river flows is necessary to enable appropriate planning and adaptation (Huntjens et al, 2012)

  • A large number of studies have looked at the potential impacts of climate change on river flows in Great Britain (GB) using the UK Climate Projections 2009 (UKCP09; Murphy et al, 2009), which provided a number of products giving information on potential future changes in a range of climatic variables up to 2100

  • A version has been configured to cover Northern Ireland and sub-catchments in the Republic of Ireland (RoI) that drain to NI rivers, on a spatial domain aligned with the GB national grid

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Summary

Introduction

Information on the potential future impacts of climate change on river flows is necessary to enable appropriate planning and adaptation (Huntjens et al, 2012). There is already evidence of increases in floods in north-west Europe and the UK (Bloschl et al, 2019), but changes in hydrological droughts are less clear (Hanel et al 2018, Rudd et al 2017). Broad-scale modelling studies suggest that parts of north-west Europe will continue to see increases in floods, with possible decreases in low flows and increases in drought duration in western/southern regions (Marx et al, 2018, Thober et al, 2018, Roudier et al 2016). A large number of studies have looked at the potential impacts of climate change on river flows in Great Britain (GB) using the UK Climate Projections 2009 (UKCP09; Murphy et al, 2009), which provided a number of products giving information on potential future changes in a range of climatic variables up to 2100.

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