A new NASA study shows that a loss of water from the rocks of California’s Sierra Nevada caused the mountain range to rise nearly an inch (24 millimeters) in height during the drought years from October 2011 to October 2015. In the two following years of more abundant snow and rainfall, the mountains have regained about half as much water in the rock as they had lost in the preceding drought and have fallen about half an inch (12 millimeters) in height.
“This suggests that the solid Earth has a greater capacity to store water than previously thought,” said research scientist Donald Argus of NASA’s Jet Propulsion Laboratory in Pasadena, California, who led the study. Significantly more water was lost from cracks and soil within fractured mountain rock during drought and gained during heavy precipitation than hydrology models show.
Argus is giving a talk on the new finding today at the American Geophysical Union’s fall conference in New Orleans.
The research team used advanced data-processing techniques on data from 1,300 GPS stations in the mountains of California, Oregon, and Washington, collected from 2006 through October 2017. These research-quality GPS receivers were installed as part of the National Science Foundation’s Plate Boundary Observatory to measure subtle tectonic motion in the region’s active faults and volcanoes. They can monitor elevation changes within less than a tenth of an inch (a few millimeters).
The team found that the amount of water lost from within fractured mountain rock in 2011-2015 amounted to 10.8 cubic miles (45 cubic kilometers) of water. This water is too inaccessible to be used for human purposes, but for comparison, the amount is 45 times as much water as Los Angeles currently uses in a year.
JPL water scientist Jay Famiglietti, who collaborated on the research, said the finding solves a mystery for hydrologists. “One of the major unknowns in mountain hydrology is what happens below the soil. How much snowmelt percolates through fractured rock straight downward into the core of the mountain? This is one of the key topics that we addressed in our study.”
Earth’s surface falls locally when it is weighed down with water and rebounds when the weight disappears. Many other factors also change the ground level, such as the movement of tectonic plates, volcanic activity, high- and low-pressure weather systems, and Earth’s slow rebound from the last ice age. The team corrected for these and other factors to estimate how much of the height increase was solely due to water loss from rock.
Before this study, scientists’ leading theories for the growth of the Sierra were tectonic uplift or Earth rebounding from extensive groundwater pumping in the adjoining California Central Valley. Argus calculated that these two processes together only produced a quarter of an inch (7 millimeters) of growth — less than a third of the total.
Famiglietti said the techniques developed for this study will allow scientists to begin exploring other questions about mountain groundwater. “What does the water table look like within mountain ranges? Is there a significant amount of groundwater stored within mountains? We just don’t have answers yet, and this study identifies a set of new tools to help us get them.”
A paper on the research, titled “Sustained water loss in California’s mountain ranges during the severe drought from 2012 through 2015 inferred from GPS,” was published in the Journal of Geophysical Research: Solid Earth.
Reference: “Sustained water loss in California’s mountain ranges during severe drought from 2012 through 2015 inferred from GPS” by Donald F. Argus, Felix W. Landerer, David N. Wiese, Hilary R. Martens, Yuning Fu, James S. Famiglietti, Brian F. Thomas, Thomas G. Farr, Angelyn W. Moore and Michael M. Watkins, 24 November 2017, Journal of Geophysical Research: Solid Earth.
DOI: 10.1002/2017JB014424
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1 Comment
That this happened to the Sierra Nevada range in a relatively short time makes me wonder how rapidly the post-glacial rebound took place at the end of the last ice age in the Great Lakes region.