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首页> 外文期刊>Journal of earth system science >Potential impacts of climate change on groundwater resources: A multi-regional modelling assessment
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Potential impacts of climate change on groundwater resources: A multi-regional modelling assessment

机译:气候变化对地下水资源的潜在影响:多区域模拟评估

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The complexity of understanding the groundwater resources in relation to climate change is caused by direct and indirect effects of climate change on hydrological processes. The study herein aims at implementing a physically based groundwater model to investigate the effects of climate change on groundwater system under 15 general circulation models (GCMs) in a semi-arid region from 2020 to 2044. A non-parametric probability density function estimator was used to quantify the level of uncertainties in the simulations. The method was applied to an area of 2073 km$^{2}$ in southwest Iran, consisting of five plains: western Dez, eastern Dez, Sabili, Deymche and Lor. The results indicate that there is a decline in the recharge in April, May, June and October. The range of changes in the recharge was determined to be between $-$10% and +13% in the Sabili plain, $-$6% and +10% in the Deymche plain, $-$4% and +10% in the western-Dez plain, $-$6% and +26% in the eastern-Dez plain, and $-$40% and +100% in the Lor plain. The most significant decline in the groundwater level occurred in the Sabili plain in September. The largest uncertainty in the simulation of recharge under GCM scenarios was determined to be in August, September and December. This study highlights that climate change can have a significant effect on groundwater resources in the region that reinforces the need for groundwater management plans and a long-term perspective.
机译:了解与气候变化有关的地下水资源的复杂性是由于气候变化对水文过程的直接和间接影响所致。本文的研究旨在实施基于物理的地下水模型,以研究2020年至2044年半干旱地区15种普通循环模型(GCM)下气候变化对地下水系统的影响。使用了非参数概率密度函数估计器量化模拟中的不确定性水平。该方法应用于伊朗西南部2073 km $ ^ {2} $的区域,该区域由五个平原组成:西部的Dez,东部的Dez,Sabili,Deymche和Lor。结果表明,4月,5月,6月和10月的充值有所下降。萨比利平原的充值变化范围确定为$-$ 10%至+ 13%,Deymche平原为$-$ 6%至+ 10%,西部地区为$-$ 4%至+ 10%。 Dez平原,东德斯平原为$-$ 6%和+ 26%,Lor平原为$-$ 40%和+ 100%。地下水位最大的下降发生在9月的萨比利平原。在GCM场景下模拟补给的最大不确定性被确定为8月,9月和12月。这项研究强调,气候变化可能对该地区的地下水资源产生重大影响,从而增强了对地下水管理计划和长期前景的需求。

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