Drought was harder to see as 2011 drew to a close. With the return of winter, rains began to fall and temperatures dropped. But the drought was still there, lingering beneath the surface. It was still apparent to hydrologists who test the wells that plunge deep into underground aquifers.
In Nebraska, Brian Wardlow and colleagues at the National Drought Mitigation Center watched the drought long before and after the average citizen paid heed. Wardlow develops satellite-based products that experts use—along with more traditional ground observations—to assess the severity of drought. Looking at measurements from the satellites, Wardlow could see broad-scale changes in groundwater supplies at varying depths over large swaths of the South.
Measurements of underground water storage (aquifers)—rather than surface water (lakes, rivers, etc.)—reveal the long-term effects of drought. This map shows ground water conditions in the U.S. during the week of November 28, 2011, compared to the long-term average. A time-series animation shows the evolution of ground water from 2002 to 2012. (Map by Chris Poulsen, National Drought Mitigation Center, based on data from the GRACE science team.)
After a year without much rain, it was no surprise that the drought lingered below the land’s surface. “Groundwater takes a long time to be depleted, but it takes a long time to be recharged as well,” says Wardlow, a remote sensing specialist at the University of Nebraska–Lincoln. From experience, he expected regional groundwater supplies to be diminished. But this time he could see it in greater detail than traditional well measurements had ever provided....
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