Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate

Abstract Climate change threatens the sustainable use of groundwater resources worldwide by affecting future recharge rates. However, assessments of global warming's impact on groundwater recharge at local scales are lacking. This study provides a continental‐scale assessment of groundwater rec...

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Main Authors: Rohini Kumar, Luis Samaniego, Stephan Thober, Oldrich Rakovec, Andreas Marx, Niko Wanders, Ming Pan, Falk Hesse, Sabine Attinger
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Earth's Future
Online Access:https://doi.org/10.1029/2024EF005020
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author Rohini Kumar
Luis Samaniego
Stephan Thober
Oldrich Rakovec
Andreas Marx
Niko Wanders
Ming Pan
Falk Hesse
Sabine Attinger
author_facet Rohini Kumar
Luis Samaniego
Stephan Thober
Oldrich Rakovec
Andreas Marx
Niko Wanders
Ming Pan
Falk Hesse
Sabine Attinger
author_sort Rohini Kumar
collection DOAJ
description Abstract Climate change threatens the sustainable use of groundwater resources worldwide by affecting future recharge rates. However, assessments of global warming's impact on groundwater recharge at local scales are lacking. This study provides a continental‐scale assessment of groundwater recharge changes in Europe, past, present, and future, at a (5×5) km2 resolution under different global warming levels (1.5, 2.0, and 3.0 K). Utilizing multi‐model ensemble simulations from four hydrologic and land‐surface models (HMs), our analysis incorporates E‐OBS observational forcing data (1970–2015) and five bias‐corrected and downscale climate model (GCMs) data sets covering the near‐past to future climate conditions (1970–2100). Results reveal a north‐south polarization in projected groundwater recharge change: declines over 25%–50% in the Mediterranean and increases over 25% in North Scandinavia at high warming levels (2.0–3.0 K). Central Europe shows minimal changes (±5%) with larger uncertainty at lower warming levels. The southeastern Balkan and Mediterranean region exhibited high sensitivity to warming, with changes nearly doubling between 1.5 and 3.0 K. We identify greater uncertainty from differences among GCMs, though significant uncertainties due to HMs exist in regions like the Mediterranean, Nordic, and Balkan areas. The findings highlight the importance of using multi‐model ensembles to assess future groundwater recharge changes in Europe and emphasize the need to mitigate impacts in higher warming scenarios.
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issn 2328-4277
language English
publishDate 2025-01-01
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spelling doaj-art-e6f70d1025ca44bfb589ca0ee5a3174a2025-01-28T15:40:37ZengWileyEarth's Future2328-42772025-01-01131n/an/a10.1029/2024EF005020Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming ClimateRohini Kumar0Luis Samaniego1Stephan Thober2Oldrich Rakovec3Andreas Marx4Niko Wanders5Ming Pan6Falk Hesse7Sabine Attinger8Department Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyDepartment Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyDepartment Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyDepartment Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyDepartment Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyDepartment of Physical Geography Utrecht University Utrecht The NetherlandsCenter for Western Weather and Water Extremes Scripps Institution of Oceanography University of California San Diego La Jolla CA USAUmweltbundesamt Dessau‐Rosslau GermanyDepartment Computational Hydrosystems Helmholtz Centre for Environmental Research GmbH—UFZ Leipzig GermanyAbstract Climate change threatens the sustainable use of groundwater resources worldwide by affecting future recharge rates. However, assessments of global warming's impact on groundwater recharge at local scales are lacking. This study provides a continental‐scale assessment of groundwater recharge changes in Europe, past, present, and future, at a (5×5) km2 resolution under different global warming levels (1.5, 2.0, and 3.0 K). Utilizing multi‐model ensemble simulations from four hydrologic and land‐surface models (HMs), our analysis incorporates E‐OBS observational forcing data (1970–2015) and five bias‐corrected and downscale climate model (GCMs) data sets covering the near‐past to future climate conditions (1970–2100). Results reveal a north‐south polarization in projected groundwater recharge change: declines over 25%–50% in the Mediterranean and increases over 25% in North Scandinavia at high warming levels (2.0–3.0 K). Central Europe shows minimal changes (±5%) with larger uncertainty at lower warming levels. The southeastern Balkan and Mediterranean region exhibited high sensitivity to warming, with changes nearly doubling between 1.5 and 3.0 K. We identify greater uncertainty from differences among GCMs, though significant uncertainties due to HMs exist in regions like the Mediterranean, Nordic, and Balkan areas. The findings highlight the importance of using multi‐model ensembles to assess future groundwater recharge changes in Europe and emphasize the need to mitigate impacts in higher warming scenarios.https://doi.org/10.1029/2024EF005020
spellingShingle Rohini Kumar
Luis Samaniego
Stephan Thober
Oldrich Rakovec
Andreas Marx
Niko Wanders
Ming Pan
Falk Hesse
Sabine Attinger
Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
Earth's Future
title Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
title_full Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
title_fullStr Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
title_full_unstemmed Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
title_short Multi‐Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
title_sort multi model assessment of groundwater recharge across europe under warming climate
url https://doi.org/10.1029/2024EF005020
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