Groundwater Level Declines Are Widespread, But Not Inevitable

Exploring acceleration in groundwater declines in aquifers around the world, and cases of recovery.

The primary water source for countless homes, farms, and cities is under threat. Unsustainable groundwater withdrawals are resulting in groundwater declines that threaten ecosystems and economies alike. New research published today in Nature reveals an acceleration in rates of groundwater depletion, emphasizing the need for comprehensive strategies to safeguard groundwater resources.

In this new study—led by researchers at the University of California, Santa Barbara, ETH Zurich, Rutgers University, King Abdulaziz University, and University College London—scientists compiled a global database of groundwater-level measurements to assess trends in 1,693 aquifers from over 170,000 wells. Their analysis shows that groundwater declines are not only widespread, but that rates of decline have accelerated over the past four decades in many aquifers.

Cuyama Valley in California, where groundwater levels are in decline

Cuyama Valley in California, where groundwater levels are in decline

Groundwater depletion poses a threat to agricultural production and domestic water access. Nearly half of all water withdrawals for global irrigation are supplied by groundwater, meaning groundwater depletion can jeopardize crop yields. For example, recent research has suggested that falling groundwater levels in parts of India could reduce agricultural production by as much as 68% (source: Jain et al., 2021).

Beyond food production, billions of people rely on groundwater wells to meet their needs, underscoring the magnitude of this threat.

Water well on farmland in Chennai, India

Groundwater Level Declines Accelerate

The analysis of 300 million groundwater level observations spanning forty years (1980 to 2022) found that, in 30 percent of these aquifer systems, the rate of groundwater level decline was faster in the early 21st century relative to the 1980s and 1990s. This finding demonstrates an acceleration in the rates of groundwater decline.

Changes in global precipitation patterns help to explain some of these accelerated declines. Reductions in precipitation can cause groundwater levels to fall by decreasing aquifer recharge rates (a direct impact of climate on groundwater) or by elevating demand for groundwater during droughts (an indirect impact of climate on groundwater; source: Taylor et al. 2013).

This analysis shows that over 80% of aquifers experiencing accelerated declines are located in areas where precipitation declined over the past 40 years, highlighting potential links between changes in climate trends, and groundwater use and replenishment.

Cultivation in Iran's Western Qazvin Plain Aquifer.

Cultivation in Iran's Western Qazvin Plain Aquifer.

Accelerated depletion of aquifers has consequences for communities across the globe.

In Iran’s Western Qazvin Plain Aquifer, an acceleration in the rate of groundwater level decline is driven by population growth, increased agricultural production, and abstraction of groundwater (source: Yazdi et al. 2021). From 1939 to 2009, the total amount of annual groundwater extraction increased from 1 million to 30 million cubic meters per year (source: Babaee et al., 2019). As a result, land subsidence has intensified and increased the risk of damage to buildings and other infrastructure.

In southeastern Spain, accelerated declines in groundwater levels have caused seawater to contaminate coastal aquifers (source: GimĂ©nez & Morell, 1997). This salinization of groundwater can render groundwater unfit for use, and jeopardize agricultural production and domestic access to water supplies as wells are abandoned.

Seawater intrusion in aquifer, southeastern Spain.

Seawater intrusion in aquifer, southeastern Spain.

The acceleration of groundwater depletion is evidence that current groundwater uses are unsustainable in some places, suggesting a need for interventions to protect agricultural production and domestic water access.

The second finding of this recent research highlights specific areas that have turned things around via interventions that have slowed, stopped, or even reversed groundwater depletion.

Central Arizona Project to divert water from the Colorado river to refill basin.

Cases of Hope

Specifically, this research also identifies cases where the groundwater depletion of the 1980s and 90s was halted, allowing aquifers to refill. These cases highlight potential solutions that have addressed the needs of specific aquifers and reversed groundwater declines.

Intervention strategies spanning from engineering to water policy have been successful in mitigating the impacts of withdrawals and climatic drivers on groundwater levels.

Albuquerque, New Mexico

Rio Grande in Albuquerque, New Mexico

Rio Grande in Albuquerque, New Mexico

Since the 1970s, the population of Albuquerque has more than doubled, increasing groundwater demand for municipal purposes. As groundwater use rose, groundwater levels in the Albuquerque Basin fell.

However, in 2008 the San-Juan Chama Project provided an inter-basin transfer of surface water from the Colorado River Basin into the Rio Grande Basin to meet the water needs of Albuquerque.

Depth to groundwater in Albuquerque Basin from 1980 to 2022. Declines in the water table slowed and then began to reverse in the early 2000s.

Depth to groundwater in Albuquerque Basin from 1980 to 2022. Declines in the water table slowed and then began to reverse in the early 2000s.

The project successfully reduced the demand for groundwater and, since 2010, groundwater levels have recovered.

Abbas -e Sharghi Basin, Iran

Satellite image of Karkheh Dam (top) and Abbas -e Sharghi Basin (left), near Emamzadeh Abbas, Iran.

Satellite image of Karkheh Dam (top) and Abbas -e Sharghi Basin (left), near Emamzadeh Abbas, Iran.

In Iran’s Abbas -e Sharghi Basin, water levels began declining in the mid-20th century due to the extensive use of groundwater wells for agricultural purposes.

However, these declines were reversed following water diversions to the basin from the Karkheh Dam, and the construction of an extensive irrigation network (source: Karami et al., 2015). Commencing in 2005, the transfer of water from the dam reservoir, coupled with the construction of irrigation systems, has facilitated aquifer recharge and reduced groundwater withdrawals.

Depth to groundwater level from 1980s to 2022. Rapid declines of the water table were reversed in the early 2000s following surface water transfers to the aquifer.

Depth to groundwater level from 1980s to 2022. Rapid declines of the water table were reversed in the early 2000s following surface water transfers to the aquifer.

These factors have resulted in a such substantial increases in groundwater levels that the water table may now be too shallow for efficient agriculture, due to waterlogging and soil salinization issues that are linked to the near-surface nature of the groundwater (source: Karimi et al., 2017)

Lower Chao Phraya Basin, Thailand

Chao Phraya River in Bangkok, Thailand.

Chao Phraya River in Bangkok, Thailand.

Another pathway to groundwater recovery comes in the form of groundwater policies. In Thailand's Bangkok Basin, the implementation of regulatory measures such as groundwater pumping fees and licensing of wells has been credited for the 21st century recovery of groundwater levels (source: Foster and Buapeng, 2008).

Depth to groundwater in Bangkok Basin from 1980 to 2010. Rapid declines of the water table were reversed following the implementation of better groundwater management practices in the early 21st century.

Depth to groundwater in Bangkok Basin from 1980 to 2010. Rapid declines of the water table were reversed following the implementation of better groundwater management practices in the early 21st century.

Following the implementation of mitigation strategies, groundwater levels have been increasing steadily since the year 2000.

While these cases of recovery reveal that interventions of suitable scale can reverse groundwater depletion, they represent the exception rather than the rule. Cases of rapid and accelerating groundwater level declines far outnumber cases where interventions have addressed groundwater depletion.

Concentrated efforts are needed to address global groundwater depletion. However, continued groundwater depletion is not an inevitability. This research shows the potential for effective water management practices to reverse groundwater declines and ensure that farms, industries, and communities have access to groundwater for generations to come.

To read more about this groundwater research you can access this freely available research in Nature with the headline: Rapid groundwater declines in many aquifers globally but cases of recovery. More information about this research is also available here.

This research was supported by the Hydrological Science program of the National Science Foundation, the Canadian Institute for Advanced Research, and the Zegar Family Foundation.