4.8 Article

Divergent effects of climate change on future groundwater availability in key mid-latitude aquifers

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NATURE COMMUNICATIONS
卷 11, 期 1, 页码 -

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NATURE PUBLISHING GROUP
DOI: 10.1038/s41467-020-17581-y

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资金

  1. IGEM project Impact of Groundwater in Earth system Models
  2. French Agence Nationale de la Recherche (ANR) [ANR-14-CE01-0018-01]
  3. Taiwanese Ministry of Science and Technology
  4. NASA GRACE Science Team
  5. Research and Technology Development program of the NASA Jet Propulsion Laboratory at the California Institute of Technology
  6. NASA
  7. [MOST 104-2923-M-002-002-MY4]
  8. [MOST 106-2111-M-002-010-MY4]
  9. Agence Nationale de la Recherche (ANR) [ANR-14-CE01-0018] Funding Source: Agence Nationale de la Recherche (ANR)

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Groundwater provides critical freshwater supply, particularly in dry regions where surface water availability is limited. Climate change impacts on GWS (groundwater storage) could affect the sustainability of freshwater resources. Here, we used a fully-coupled climate model to investigate GWS changes over seven critical aquifers identified as significantly distressed by satellite observations. We assessed the potential climate-driven impacts on GWS changes throughout the 21(st) century under the business-as-usual scenario (RCP8.5). Results show that the climate-driven impacts on GWS changes do not necessarily reflect the long-term trend in precipitation; instead, the trend may result from enhancement of evapotranspiration, and reduction in snowmelt, which collectively lead to divergent responses of GWS changes across different aquifers. Finally, we compare the climate-driven and anthropogenic pumping impacts. The reduction in GWS is mainly due to the combined impacts of over-pumping and climate effects; however, the contribution of pumping could easily far exceed the natural replenishment. Climate change may impact groundwater storage and thus the availability of freshwater resources. Here the authors use climate models to examine seven aquifers and find that storage changes are primarily the result of enhancement of evapotranspiration, reduction in snowmelt, and over-pumping rather than long-term precipitation changes.

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