Multi-Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F25%3A102099" target="_blank" >RIV/60460709:41330/25:102099 - isvavai.cz</a>
Výsledek na webu
<a href="https://doi.org/10.1029/2024EF005020" target="_blank" >https://doi.org/10.1029/2024EF005020</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2024EF005020" target="_blank" >10.1029/2024EF005020</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Multi-Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
Popis výsledku v původním jazyce
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 (5x5) $(5times 5)$ km2 ${text{km}}<^>{2}$ 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 (+/- $pm $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.
Název v anglickém jazyce
Multi-Model Assessment of Groundwater Recharge Across Europe Under Warming Climate
Popis výsledku anglicky
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 (5x5) $(5times 5)$ km2 ${text{km}}<^>{2}$ 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 (+/- $pm $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.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10501 - Hydrology
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2025
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Earths Future
ISSN
2328-4277
e-ISSN
2328-4277
Svazek periodika
13
Číslo periodika v rámci svazku
JAN 2025
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
19
Strana od-do
1-19
Kód UT WoS článku
001406941100001
EID výsledku v databázi Scopus
2-s2.0-85216299458