 News release: 2013-154 May 2, 2013 NASA Opens New Era in Measuring Western U.S. Snowpack 
The full version of this story with accompanying images is at: http://www.jpl.nasa.gov/news/news.php?release=2013-154&cid=release_2013-154 PASADENA, Calif. - A new NASA airborne mission has created the first maps of the entire snowpack of two major mountain watersheds in California and Colorado, producing the most accurate measurements to date of how much water they hold. The data from NASA's Airborne Snow Observatory mission will be used to estimate how much water will flow out of the basins when the snow melts. The data-gathering technology could improve water management for 1.5 billion people worldwide who rely on snowmelt for their water supply. "The Airborne Snow Observatory is on the cutting edge of snow remote-sensing science," said Jared Entin, a program manager in the Earth Science Division at NASA Headquarters in Washington. "Decision makers like power companies and water managers now are receiving these data, which may have immediate economic benefits." The mission is a collaboration between NASA's Jet Propulsion Laboratory, Pasadena, Calif., and the California Department of Water Resources in Sacramento. A Twin Otter aircraft carrying NASA's Airborne Snow Observatory began a three-year demonstration mission in April that includes weekly flights over the Tuolumne River Basin in California's Sierra Nevada and monthly flights over Colorado's Uncompahgre River Basin. The flights will run through the end of the snowmelt season, which typically occurs in July. The Tuolumne watershed and its Hetch Hetchy Reservoir are the primary water supply for San Francisco. The Uncompahgre watershed is part of the Upper Colorado River Basin that supplies water to much of the western United States. The mission's principal investigator, Tom Painter of JPL, said the mission fills a critical need in an increasingly thirsty world, initially focusing on the western United States, where snowmelt provides more than 75 percent of the total freshwater supply. "Changes in and pressure on snowmelt-dependent water systems are motivating water managers, governments and others to improve understanding of snow and its melt," Painter said. "The western United States and other regions face significant water resource challenges because of population growth and faster melt and runoff of snowpacks caused by climate change. NASA's Airborne Snow Observatory combines the best available technologies to provide precise, timely information for assessing snowpack volume and melt." The observatory's two instruments measure two properties most critical to understanding snowmelt runoff and timing. Those two properties had been mostly unmeasured until now. A scanning lidar system from the Canadian firm Optech Inc. of Vaughan, Ontario, measures snow depth with lasers to determine the first property, snow water equivalent. Snow water equivalent represents the amount of water in the snow on a mountain. It is used to calculate the amount of water that will run off. An imaging spectrometer built by another Canadian concern, ITRES of Calgary, Alberta, measures the second property, snow albedo. Snow albedo represents the amount of sunlight reflected and absorbed by snow. Snow albedo controls the speed of snowmelt and timing of its runoff. By combining these data, scientists can tell how changes in the absorption of sunlight cause snowmelt rates to increase. The Airborne Snow Observatory flies at an altitude of 17,500 to 22,000 feet (5,334 to 6,705 meters) to produce frequent maps that scientists can use to monitor changes over time. It can calculate snow depth to within about 4 inches (10 centimeters) and snow water equivalent to within five percent. Data are processed on the ground and made available to participating water managers within 24 hours. Before now, Sierra Nevada snow water equivalent estimates have been extrapolated from monthly manual ground snow surveys conducted from January through April. These survey sites are sparsely located, primarily in lower to middle elevations that melt free of snow each spring, while snow remains at higher elevations. Water managers use these survey data to forecast annual water supplies. The information affects decisions by local water districts, agricultural interests and others. The sparse sampling can lead to large errors. In contrast, the NASA observatory can map all the snow throughout the entire snowmelt season. "The Airborne Snow Observatory is providing California water managers the first near-real-time, comprehensive determination of basin-wide snow water equivalent," said Frank Gehrke, mission co-investigator and chief of the California Cooperative Snow Surveys Program for the California Department of Water Resources. "Integrated into models, these data will enhance the state's reservoir operations, permitting more efficient flood control, water supply management and hydroelectric power generation." Gehrke said the state will continue to conduct manual surveys while it incorporates the Airborne Snow Observatory data. "The snow surveys are relatively inexpensive, help validate observatory data and provide snow density measurements that are key to reducing errors in estimating snow water equivalent," he said. Painter plans to expand the airborne mapping program to the entire Upper Colorado River Basin and Sierra Nevada. "We believe this is the future of water management in the western United States," he said. For more information about the Airborne Snow Observatory, visit: http://aso.jpl.nasa.gov/ . For more on NASA's Airborne Science program, visit: http://airbornescience.nasa.gov . The California Institute of Technology in Pasadena manages JPL for NASA. Alan Buis 818-354-0474 Jet Propulsion Laboratory, Pasadena, Calif. Alan.buis@xxxxxxxxxxxx Steve Cole 202-358-0918 NASA Headquarters, Washington Stephen.e.cole@xxxxxxxx Elizabeth Scott 916-712-3904 California Department of Water Resources, Sacramento Elizabeth.Scott@xxxxxxxxxxxx - end - |
