One-Third Of The World’s Largest Groundwater Sources Are In Serious Trouble: Study
The earth’s biggest groundwater basins are being depleted far more quickly than previously believed, according to two new studies by the University of California, Irvine (UCI).
The studies used data from NASA’s Gravity Recovery and Climate Experiment (GRACE) satellites gathered between 2003 and 2013 to examine the 37 largest aquifers on the planet. Twenty-one of those aquifers have exceeded their sustainability “tipping points,” meaning they lose more water every year than is being naturally replenished through processes like rainfall or snow melt, said Jay Famiglietti, senior water scientist at NASA Jet Propulsion Laboratory and principal investigator in the two studies.
Out of those 21, eight were found to be “overstressed,” meaning there is “nearly no natural replenishment” to restore water used by humans, according to a statement from UCI. Another five were designated “extremely or highly stressed,” signifying that they are “still in trouble” but have “some water flowing back into them.”
Image credit: UC Irvine/NASA/JPL-Caltech
Among those classified as “highly stressed” is the California Central Valley Aquifer System. In dry years, groundwater typically supplies 46 percent or more of the state’s water, according to the California Department of Water Resources. California is now in its fourth year of exceptional drought. Many communities rely on groundwater exclusively for their water needs, the department noted.
The world’s most overstressed groundwater source, according to researchers, is the Arabian Aquifer System, which supplies water for more than 60 million people.
Researchers used readings from NASA’s two GRACE satellites, which measure variations in the earth’s gravitational pull, Famiglietti told The Huffington Post. When an area either gains or loses a large volume of water, the change in mass allows the satellites pick up the difference in the gravitational pull. This lets researchers determine the rate at which large —> Read More