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Groundwater-fed irrigation of Boro rice during the dry season in the Ganges-Brahmaputra Basin

Flood discharge from 2015-16 El Niño rains providing episodic recharge to a wellfield in central, semi-arid Tanzania, the only perennial source of water to nation’s capital, Dodoma

Fewer of the world’s large aquifers are depleting than previously estimated, according to a new study by the University of Sussex and UCL.

Groundwater, the world’s largest distributed store of freshwater, plays a critical role in supplying water for irrigation, drinking and industry, and sustaining vital ecosystems.

Previous global studies of changes in groundwater storage, estimated using data from the GRACE (Gravity Recovery and Climate Experiment) satellite mission and global models, have concluded that intensifying human water withdrawals in the majority of the world’s large aquifer systems are causing a sustained reduction in groundwater storage, depleting groundwater resources.

Yet this new study, published in Earth System Dynamics, reveals that depletion is not as widespread as reported, and that replenishment of groundwater storage depends upon extreme rainfall that is increasing under global climate change.

Lead author, Dr Mohammad Shamsudduha, Lecturer in Physical Geography and a member of the Sussex Sustainability Research Programme at the University of Sussex, said: “The cloud of climate change has a silver lining for groundwater resources as it favours greater replenishment from episodic, extreme rainfalls in some aquifers located around the world mainly in dry environments. This new analysis provides a benchmark alongside conventional, ground-based monitoring of groundwater levels to assess changes in water storage in aquifers over time. This information is essential to inform sustainable management of groundwater resources.”

This new study updates and extends previous analyses, accounting for strong seasonality in groundwater storage in the analysis of trends. It shows that a minority (only 5) of the world’s 37 large aquifers is undergoing depletion that requires further attention for better management.

Co-author, Professor of Hydrogeology, Richard Taylor from UCL Geography, said: “The findings do not deny that groundwater depletion is occurring in many parts of the world but that the scale of this depletion, frequently associated with irrigation in drylands, is more localised than past studies have suggested and often occurs below a large (~100 000 km²) ‘footprint’ of mass changes tracked by a pair of GRACE satellites.”

For the majority, trends are non-linear and irregular, exhibiting considerable variability in volume over time. The study shows further that variability in groundwater storage in drylands is influenced positively and episodically by years of extreme (>90^th percentile) precipitation.

For example, in the Great Artesian Basin of Australia, extreme seasonal rainfall over two successive summers in 2010 and 2011 increased groundwater storage there by ~90 km³, more than ten times total annual freshwater withdrawals in the UK. Elsewhere in the Canning Basin of Australia, however, groundwater depletion is occurring at a rate of 4.4 km³ each year that is associated with its use in the extraction of iron ore.

To avoid continued depletion of aquifers, the study promotes sustainable groundwater withdrawals through augmented replenishments from extreme rainfall and ‘managed aquifer recharge’ practices.

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