How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?

How climate change will affect the spatial coherence of droughts is a key question that water managers must answer in order to adopt strategies to mitigate impacts on water resources. Water transfers from regions with excess to those in deficit are fundamental to such strategies, but only possible i...

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Main Authors: Maliko Tanguy, Amulya Chevuturi, Ben P Marchant, Jonathan D Mackay, Simon Parry, Jamie Hannaford
Format: Article
Language:English
Published: IOP Publishing 2023-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/acd655
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author Maliko Tanguy
Amulya Chevuturi
Ben P Marchant
Jonathan D Mackay
Simon Parry
Jamie Hannaford
author_facet Maliko Tanguy
Amulya Chevuturi
Ben P Marchant
Jonathan D Mackay
Simon Parry
Jamie Hannaford
author_sort Maliko Tanguy
collection DOAJ
description How climate change will affect the spatial coherence of droughts is a key question that water managers must answer in order to adopt strategies to mitigate impacts on water resources. Water transfers from regions with excess to those in deficit are fundamental to such strategies, but only possible if both regions are not simultaneously under drought conditions—these relationships could change in a warming world. Here, we use future simulations (under RCP8.5) of streamflow (186 catchments) and groundwater level (41 boreholes) from the Enhanced Future Flows and Groundwater (eFLaG) dataset to analyse the projected change in the spatial coherence of hydrological droughts at a national scale, with Great Britain as an example. Joint and conditional probabilities of two regions being in drought simultaneously are used to characterise the spatial coherence. The results are sensitive to various uncertainties, including the way drought is defined. However, some key findings emerge. In particular, for droughts defined based on current conditions, our results show that the spatial coherence of streamflow droughts for the ‘far future’ (2050–2089) is expected to increase during the summer everywhere in the country. During the winter, however, spatial coherence may only increase in the South-East, where the sharpest rise in winter droughts is likely to occur. The coherence between groundwater and streamflow droughts shows a more mixed picture, dependant on season and region. One important observation is that, in the South-East during the summer, the proportion of streamflow droughts that coincide with groundwater droughts is expected to decrease. These results provide a valuable insight for water managers to help inform their long-term strategy to overcome future impacts of droughts, including the feasibility of inter-region water transfers and conjunctive use (surface and groundwater) schemes. This flexible methodology has the potential to be applied in other parts of the world to help shape strategic regional and national investments to increase resilience to droughts.
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spelling doaj.art-0385ba19c1b34cb8b53819411d0d2aeb2023-08-09T15:16:14ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-0118606404810.1088/1748-9326/acd655How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?Maliko Tanguy0https://orcid.org/0000-0002-1516-6834Amulya Chevuturi1https://orcid.org/0000-0003-2815-7221Ben P Marchant2https://orcid.org/0000-0001-7633-1920Jonathan D Mackay3https://orcid.org/0000-0003-4373-5747Simon Parry4https://orcid.org/0000-0002-7057-4195Jamie Hannaford5https://orcid.org/0000-0002-5256-3310UK Centre for Ecology & Hydrology (UKCEH) , Wallingford, United KingdomUK Centre for Ecology & Hydrology (UKCEH) , Wallingford, United KingdomBritish Geological Survey (BGS) , Keyworth, United KingdomBritish Geological Survey (BGS) , Keyworth, United Kingdom; School of Geography, Earth and Environmental Sciences, University of Birmingham , Edgbaston, Birmingham, United KingdomUK Centre for Ecology & Hydrology (UKCEH) , Wallingford, United KingdomUK Centre for Ecology & Hydrology (UKCEH) , Wallingford, United Kingdom; Irish Climate Analysis and Research UnitS (ICARUS), Maynooth University , Maynooth, IrelandHow climate change will affect the spatial coherence of droughts is a key question that water managers must answer in order to adopt strategies to mitigate impacts on water resources. Water transfers from regions with excess to those in deficit are fundamental to such strategies, but only possible if both regions are not simultaneously under drought conditions—these relationships could change in a warming world. Here, we use future simulations (under RCP8.5) of streamflow (186 catchments) and groundwater level (41 boreholes) from the Enhanced Future Flows and Groundwater (eFLaG) dataset to analyse the projected change in the spatial coherence of hydrological droughts at a national scale, with Great Britain as an example. Joint and conditional probabilities of two regions being in drought simultaneously are used to characterise the spatial coherence. The results are sensitive to various uncertainties, including the way drought is defined. However, some key findings emerge. In particular, for droughts defined based on current conditions, our results show that the spatial coherence of streamflow droughts for the ‘far future’ (2050–2089) is expected to increase during the summer everywhere in the country. During the winter, however, spatial coherence may only increase in the South-East, where the sharpest rise in winter droughts is likely to occur. The coherence between groundwater and streamflow droughts shows a more mixed picture, dependant on season and region. One important observation is that, in the South-East during the summer, the proportion of streamflow droughts that coincide with groundwater droughts is expected to decrease. These results provide a valuable insight for water managers to help inform their long-term strategy to overcome future impacts of droughts, including the feasibility of inter-region water transfers and conjunctive use (surface and groundwater) schemes. This flexible methodology has the potential to be applied in other parts of the world to help shape strategic regional and national investments to increase resilience to droughts.https://doi.org/10.1088/1748-9326/acd655droughtclimate changespatial coherencewater resourcesinter-regional water transferriver flows
spellingShingle Maliko Tanguy
Amulya Chevuturi
Ben P Marchant
Jonathan D Mackay
Simon Parry
Jamie Hannaford
How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
Environmental Research Letters
drought
climate change
spatial coherence
water resources
inter-regional water transfer
river flows
title How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
title_full How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
title_fullStr How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
title_full_unstemmed How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
title_short How will climate change affect the spatial coherence of streamflow and groundwater droughts in Great Britain?
title_sort how will climate change affect the spatial coherence of streamflow and groundwater droughts in great britain
topic drought
climate change
spatial coherence
water resources
inter-regional water transfer
river flows
url https://doi.org/10.1088/1748-9326/acd655
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