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

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

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

2020
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Overview
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.