Suppr超能文献

气候变化对关键中纬度含水层未来地下水资源的影响存在差异。

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

机构信息

Department of Atmospheric Sciences, National Taiwan University, Taipei, 10617, Taiwan.

Department of Geological Sciences, The University of Texas at Austin, Austin, TX, 78712, USA.

出版信息

Nat Commun. 2020 Jul 24;11(1):3710. doi: 10.1038/s41467-020-17581-y.

Abstract

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 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.

摘要

地下水提供了关键的淡水供应,特别是在地表水供应有限的干旱地区。气候变化对地下水储存(GWS)的影响可能会影响淡水资源的可持续性。在这里,我们使用完全耦合的气候模型来研究七个被卫星观测确定为严重受损的关键含水层的地下水储量变化。我们评估了在 RCP8.5 情景下整个 21 世纪中气候驱动对地下水储量变化的潜在影响。结果表明,气候变化对地下水储量变化的影响不一定反映降水的长期趋势;相反,这种趋势可能是由于蒸散作用的增强和融雪的减少,这共同导致了不同含水层地下水储量变化的不同反应。最后,我们比较了气候驱动和人为抽汲的影响。地下水储量的减少主要是由于过度抽汲和气候影响的综合作用造成的;然而,抽汲的贡献很容易超过自然补给。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/edd3/7382464/90254f36dece/41467_2020_17581_Fig1_HTML.jpg

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验