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

Authors :
Cuthbert MO
Taylor RG
Favreau G
Todd MC
Shamsudduha M
Villholth KG
MacDonald AM
Scanlon BR
Kotchoni DOV
Vouillamoz JM
Lawson FMA
Adjomayi PA
Kashaigili J
Seddon D
Sorensen JPR
Ebrahim GY
Owor M
Nyenje PM
Nazoumou Y
Goni I
Ousmane BI
Sibanda T
Ascott MJ
Macdonald DMJ
Agyekum W
Koussoubé Y
Wanke H
Kim H
Wada Y
Lo MH
Oki T
Kukuric N
Source :
Nature [Nature] 2019 Aug; Vol. 572 (7768), pp. 230-234. Date of Electronic Publication: 2019 Aug 07.
Publication Year :
2019

Abstract

Groundwater in sub-Saharan Africa supports livelihoods and poverty alleviation <superscript>1,2</superscript> , maintains vital ecosystems, and strongly influences terrestrial water and energy budgets <superscript>3</superscript> . Yet the hydrological processes that govern groundwater recharge and sustainability-and their sensitivity to climatic variability-are poorly constrained <superscript>4,5</superscript> . 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 <superscript>4</superscript> 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 <superscript>4</superscript> 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.

Details

Language :
English
ISSN :
1476-4687
Volume :
572
Issue :
7768
Database :
MEDLINE
Journal :
Nature
Publication Type :
Academic Journal
Accession number :
31391559
Full Text :
https://doi.org/10.1038/s41586-019-1441-7