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

机译:观察到对地下水的恢复力控制撒哈拉以南非洲的气候变异性

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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:地下水在撒哈拉以南非洲支持生计和扶贫(1,2),维持重要的生态系统,强烈影响陆地水和能源预算(3)。然而,控制地下水补给和可持续性的水文过程 - 以及对气候变异性的敏感性 - 受到严重限制(4,5)。鉴于缺乏坚定的观察限制,仍有待观察到区域(4)的干燥部件下降的水资源下降的基于模型的预测是合理的。在这里,我们通过分析跨撒哈拉以南非洲的多田间地下水文文拍摄,炎症水平决定了主要的充电过程,而本地水文地质影响降水充电关系的类型和敏感性。在一些潮湿地点的补给在各种年降水量范围内变化几乎减小到5%(通过变异系数)。相比之下,其他区域显示大致线性沉淀 - 充电关系,降水阈值(每天大约10毫米或更小),用于引发充电的启动。当干燥的增加时,这些阈值往往升高,并且在旱地中的充电是通过从短暂的陆地流动的损失的重点充电越来越多的奇异。极端年度充值通常与强烈的降雨和洪水事件相关,他们自己经常受到大规模气候控制的推动。甚至在整体降水量的多年来,强烈降水,产生一些干燥的亚热带位置中的一些最大的补给。因此,我们的结果挑战了撒哈拉以南非洲地区减少水资源(4)的“高肯定”的共识。地下水在这些降水充电关系中揭示的许多领域的地下水潜在的可变性,这对于通知对气候变化影响和适应策略的可靠预测是必不可少的。

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