The record-breaking drought in Texas that has fueled wildfires, decimated crops and forced cattle sales also has reduced levels of groundwater in much of the state to the lowest levels seen in more than 60 years, according to new national maps produced by NASA and distributed by the National Drought Mitigation Center at the University of Nebraska-Lincoln.
The latest groundwater map, released in November, shows large patches of maroon over eastern Texas, indicating severely depressed groundwater levels. The maps, produced weekly by NASA's Goddard Space Flight Center in Greenbelt, Md., are publicly available on the website of the Drought Center (drought.unl.edu), headquartered at the University of Nebraska-Lincoln.
"Texas groundwater will take months or longer to recharge," says NASA hydrologist Matt Rodell, based in Goddard. "Even if we have a major rainfall event, most of the water runs off. It takes a longer period of sustained greater-than-average precipitation to recharge aquifers significantly."
The maps are based on data from NASA's Gravity Recovery and Climate Experiment (GRACE) satellites, which detect small changes in the Earth's gravity field caused by the redistribution of water on and beneath the land surface. The paired satellites travel about 137 miles apart and record small changes in the distance separating them as they encounter variations in Earth's gravitational field.
To make the maps, scientists used a sophisticated computer model that combines measurements of water storage from GRACE with a long-term meteorological dataset, to generate a continuous record of soil moisture and groundwater that stretches back to 1948. The meteorological data includes precipitation, temperature, solar radiation and other ground- and space-based measurements.
The color-coded maps show how much water is stored now as a probability of occurrence in the 63-year record. The maroon shading over eastern Texas, for example, shows that the level of dryness over the last week occurred less than 2% of the time between 1948 and the present.
The groundwater maps aren't the only maps based on GRACE data that the Drought Center publishes each week. It also distributes soil moisture maps that show moisture changes in the root zone down to about three feet below the surface, as well as surface soil moisture maps that show changes within the top inch of the land.
"These maps would be impossible to generate using only ground-based observations," Rodell says. "There are groundwater wells all around the United States, and the U.S. Geological Survey does keep records from some of those wells, but it's not spatially continuous and there are some big gaps."
The maps also offer farmers, ranchers, water resource managers and even individual homeowners a new tool to monitor the health of critical groundwater resources. "People rely on groundwater for irrigation, for domestic water supply and for industrial uses, but there's little information available on regional to national scales on groundwater storage variability and how that has responded to a drought," Rodell adds "Over a long-term dry period there will be an effect on groundwater storage and groundwater levels. It's going to drop quite a bit, people's wells could dry out, and it takes time to recover."
The maps are the result of a NASA-funded project at the Drought Center and NASA Goddard to make it easier for the weekly U.S. Drought Monitor to incorporate data from the GRACE satellites. NASA's Jet Propulsion Laboratory in Pasadena, Calif., developed GRACE and manages the mission for NASA. The groundwater and soil moisture maps are updated each Tuesday.
The maps can be viewed at http://go.unl.edu/mqk.
To learn more about the GRACE mission, go to: http://www.csr.utexas.edu/grace/.
Source: University of Nebraska-Lincoln
WATER DECLINES: Color-coded map shows how much groundwater is stored now as a probability of occurrence over 60-plus years. For instance, the maroon shade in eastern Texas reveals the level of dryness last November occurred less than 2% of the time between 1948 and the present.