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Observed controls on resilience of groundwater to climate variability in sub-Saharan Africa

机译:观察到的撒哈拉以南非洲地区地下水对气候变化的适应力控制措施

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Groundwater in sub-Saharan Africa supports livelihoods and poverty alleviation(1,2), maintains vital ecosystems, and strongly influences terrestrial water and energy budgets(3). Yet the hydrological processes that govern groundwater recharge and sustainability-and their sensitivity to climatic variability-are poorly constrained(4,5). Given the absence of firm observational constraints, it remains to be seen whether model-based projections of decreased water resources in dry parts of the region(4) are justified. Here we show, through analysis of multidecadal groundwater hydrographs across sub-Saharan Africa, that levels of aridity dictate the predominant recharge processes, whereas local hydrogeology influences the type and sensitivity of precipitation-recharge relationships. Recharge in some humid locations varies by as little as five per cent (by coefficient of variation) across a wide range of annual precipitation values. Other regions, by contrast, show roughly linear precipitation-recharge relationships, with precipitation thresholds (of roughly ten millimetres or less per day) governing the initiation of recharge. These thresholds tend to rise as aridity increases, and recharge in drylands is more episodic and increasingly dominated by focused recharge through losses from ephemeral overland flows. Extreme annual recharge is commonly associated with intense rainfall and flooding events, themselves often driven by large-scale climate controls. Intense precipitation, even during years of lower overall precipitation, produces some of the largest years of recharge in some dry subtropical locations. Our results therefore challenge the 'high certainty' consensus regarding decreasing water resources(4) in such regions of sub-Saharan Africa. The potential resilience of groundwater to climate variability in many areas that is revealed by these precipitation-recharge relationships is essential for informing reliable predictions of climate-change impacts and adaptation strategies.
机译:撒哈拉以南非洲的地下水支持生计和减贫(1,2),维持重要的生态系统,并强烈影响陆地水和能源的预算(3)。然而,控制地下水补给和可持续性的水文过程及其对气候变化的敏感性受到的约束很有限(4,5)。鉴于缺乏坚定的观测约束,该地区干旱地区水资源减少的基于模型的预测是否合理尚待观察(4)。在这里,我们通过对整个撒哈拉以南非洲地区的数十年地下水水位图的分析表明,干旱程度决定了主要的补给过程,而局部水文地质影响着降水-补给关系的类型和敏感性。在许多年降水量范围内,某些潮湿地区的补给量变化仅为5%(根据变化系数)。相比之下,其他地区则显示出大致线性的降水-补给关系,其中降水阈值(每天大约十毫米或更小)控制着补给的开始。随着干旱的增加,这些阈值趋于上升,而干旱地区的补给更是偶发性的,并且越来越多地由短暂的陆上流动造成的损失集中地补给。每年的极端补给通常与强降雨和洪水事件有关,而暴雨和洪水事件往往是由大规模气候控制驱动的。即使在总体降水量较低的年份,强降水也会在一些干燥的亚热带地区产生最大的补给年份。因此,我们的结果对撒哈拉以南非洲此类地区减少水资源的“高确定性”共识提出了挑战(4)。这些降水与补给之间的关系揭示了许多地区地下水对气候变化的潜在复原力,对于为气候变化影响和适应策略提供可靠的预测至关重要。

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