Consequently, huge sections of the population are using up groundwater without knowing when it will run out, researchers said in findings that will appear in the journal Water Resources Research and were posted online Tuesday.
“Available physical and chemical measurements are simply insufficient,” University of California Irvine professor and principal investigator Jay Famiglietti said in a statement.
“Given how quickly we are consuming the world’s groundwater reserves, we need a coordinated global effort to determine how much is left,” added Famiglietti, who is also the senior water scientist at NASA’s Jet Propulsion Laboratory.
Scientists used data from special NASA satellites to measure groundwater losses.
In the first paper, they looked at 37 of Earth’s biggest aquifers between 2003 and 2013. Eight of these were classified as “overstressed,” meaning they were being sucked dry with almost no natural replenishment to offset the usage.
Five other aquifers were determined to be “extremely or highly stressed.”
Scientists warned the situation would only worsen with climate change and population growth. The most overburdened aquifers are in the world’s driest places, where there is little natural replenishment.
“What happens when a highly stressed aquifer is located in a region with socioeconomic or political tensions that can’t supplement declining water supplies fast enough?” said Alexandra Richey, the lead author on both studies.
“We’re trying to raise red flags now to pinpoint where active management today could protect future lives and livelihoods.”
Researchers found that the Arabian Aquifer System, providing water for more than 60 million people, is the world’s most overstressed source.
The Indus Basin aquifer of northwestern India and Pakistan is the second-most overstressed, and the Murzuk-Djado Basin in northern Africa is third, scientists said.
In drought-striken California, the Central Valley aquifer was labeled as “highly stressed.”
The second paper concludes that the total remaining volume of the world’s usable groundwater is poorly known and huge discrepancies exist in estimated “time to depletion.”
“We don’t actually know how much is stored in each of these aquifers. Estimates of remaining storage might vary from decades to millennia,” Richey said.
“In a water-scarce society, we can no longer tolerate this level of uncertainty, especially since groundwater is disappearing so rapidly.” -AFP