These sponge-like freshwater reservoirs<\/a> supply water<\/a> for communities, agriculture, and surface ecosystems. But if there’s little rain<\/a> to replenish them, or too much of their water is extracted, aquifers might not recover.<\/p>\n The Sacramento Valley aquifer system, under pressure from recent droughts, is responsible for supplying part of California’s Central Valley<\/a>, where, along with the San Joaquin Valley to the south, around a quarter of the US food supply<\/a> is grown.<\/p>\n According to new data, the capacity of this aquifer has now been permanently reduced due to rapid and regular freshwater extraction over the last few years.<\/p>\n As the aquifer empties, the ground above subsides. (Larochelle et al., PNAS, 2026)<\/p>\n As the study in PNAS<\/a> shows, land subsidence above the aquifer \u2013 the drop in the layers kept in place by the underwater reservoir \u2013 has been fast and widespread enough to suggest an irreversible change.<\/p>\n “All available measurements suggest that the accelerated subsidence starting in 2021 primarily results from inelastic compaction due to groundwater extraction,” the researchers write<\/a> in their paper.<\/p>\n “On average, the ground surface does not rebound to its pre-2021 state even as groundwater levels recover with seasonal recharge at the end of 2021, indicative of irreversible deformation.”<\/p>\n The pressure within aquifers affects the land above them. As water is extracted<\/a>, the compaction of surface layers can be reversible (elastic) as the aquifer is naturally recharged, or irreversible (inelastic).<\/p>\n That latter scenario means the amount of water lost and subsequent subsidence is too great for the geological stacking to recover.<\/p>\n The aquifer’s capacity is permanently reduced, which affects how much water it can supply<\/a> in the future.<\/p>\n Analyzing the magnitude, timing, and extent of deformation in the Sacramento Valley, the researchers think that inelastic compaction has become the dominant mechanism affecting the area.<\/p>\n “Such rapid and extensive land subsidence indicates severe inelastic compaction and loss of storage capacity of the underlying aquifer system, which pose a serious threat to California’s water resources and infrastructure,” the team writes<\/a>.<\/p>\n The shaded areas show accelerated subsidence from 2021-2022, with the red lines indicating reversible decline. (Larochelle et al., PNAS, 2026)<\/p>\n To reach that conclusion, the team analyzed data from satellites equipped with navigation systems and radar instruments, giving them a wider and more accurate look \u2013 down to millimeter-level accuracy \u2013 at how the ground was deforming over the years.<\/p>\n Crucially, the satellite data spotted aquifer compaction that wouldn’t have been detected based on groundwater measurements<\/a> alone.<\/p>\n Across 2016-2020, the data showed the ground levels largely bouncing back to their earlier position.<\/p>\n After 2021, the dip in some areas was as large as 50 centimeters (almost 20 inches) per year, which is many times higher than the reversible levels seen in the years prior \u2013 around 2 centimeters (0.8 inches) per year.<\/p>\n “By imaging this sharp transition at the regional scale, our analysis demonstrates the potential of space-based monitoring for early detection of groundwater overdraft and the resulting loss of aquifer storage capacity worldwide,” write<\/a> the researchers.<\/p>\n They estimate that the loss of water storage space per year jumped up to 0.2 cubic kilometers (about 7 billion cubic feet) from 2021, around a five-fold increase compared to the previous years.<\/p>\n That’s the equivalent of around 30 percent of the annual water consumption of Los Angeles being lost in terms of capacity: a shrunken aquifer that’s not going to be able to store as much water going forward.<\/p>\n Better data might not in itself reverse global warming<\/a> or make droughts less frequent, but it can help with water management.<\/p>\n In this case, satellites caught a significant shift that a network of more than 2,500 groundwater wells didn’t reveal \u2013 but too late to do anything about it.<\/p>\n Related: ‘Most Isolated Environments’: Microplastics Are Finding Their Way Down to Deep-Sea Hydrothermal Vents<\/a><\/p>\n “Real-time monitoring of surface displacements through satellite geodesy<\/a>, which provide an integrated measure of internal deformation over the entire sedimentary column, could have enabled early detection of this sharp transition and potentially reduced storage loss through timely remedial actions,” write<\/a> the researchers.<\/p>\n “Developing such capability is especially critical in regions where in situ monitoring is unviable but groundwater resources increasingly vital.”<\/p>\n The research has been published in PNAS<\/a>.<\/p>\n This article was fact-checked by Fiona MacDonald<\/a> and edited by Clare Watson<\/a>. 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