November 29, 2004 |
The Department of the Interior’s U.S. Geological Survey is collaborating with partner agencies to conduct scientific experiments designed to evaluate the effect of a high-flow release from Glen Canyon Dam on the natural resources of the Colorado River in Grand Canyon National Park. Researchers from the USGS Grand Canyon Monitoring and Research Center are working with scientists and resource managers from Interior’s Bureau of Reclamation, Fish and Wildlife Service, National Park Service, as well as the Arizona Game and Fish Department, Northern Arizona University and other cooperators to prepare, conduct, and evaluate the experiments.
Interior Scientists Evaluate Effects of High Flow Test at Glen Canyon Dam
The Department of the Interior’s U.S. Geological Survey is collaborating with partner agencies to conduct scientific experiments designed to evaluate the effect of a high-flow release from Glen Canyon Dam on the natural resources of the Colorado River in Grand Canyon National Park.
Researchers from the USGS Grand Canyon Monitoring and Research Center are working with scientists and resource managers from Interior’s Bureau of Reclamation, Fish and Wildlife Service, National Park Service, as well as the Arizona Game and Fish Department, Northern Arizona University and other cooperators to prepare, conduct, and evaluate the experiments.
The high-flow test, which began on Sunday, Nov. 21, 2004, was launched after the successful completion of an Environmental Analysis and the issuance of a Finding of No Significant Impact statement — steps required by the National Environmental Policy Act. The EA underwent a 15-day public review and comment period that closed today.
Under the high-flow test experiment, Reclamation opened the dam’s bypass tubes for 90 hours, beginning Nov. 21. The peak high flows will run for two and one-half days (60 hours) at about 41,000 cubic-feet-per-second. The goal is to stir up and redistribute sediment from tributary rivers downstream from the dam to enlarge existing beaches and sandbars, create new ones, and distribute sediment into drainage channels.
A previous high-flow test at the dam in 1996 was designed to stir up and redistribute sediment from the bottom of the Colorado River and add it to river banks. The hypothesis underlying that test was not borne out by the results, leading scientists to believe that a more effective approach would be to redistribute tributary sediment as soon as a sufficient amount had accumulated downstream of the dam. More than a million tons of sediment had accumulated by early November, triggering the proposal from the Adaptive Management Work Group for the Nov. 21 high-flow test.
The water released during the experiment will not change the amount of water to be released over the course of the 2005 Water Year. The Annual Operating Plan calls for releasing approximately 8.23 million acre-feet of water from Glen Canyon Dam. That water is sent down river and captured in Lake Mead for use by the Lower Colorado River Basin States. The test flows are factored into that annual volume. Flows later in the year will be adjusted downward to factor in the additional water released between Nov. 21 and Nov. 25, 2004.
The science experiments focus on sediment distribution, native fish and food for aquatic animals. The results of the experiments will be used to evaluate the use of high flows to redistribute tributary sediment as a management tool for the preservation and restoration of natural and cultural resources in the Colorado River corridor below Glen Canyon Dam.
Colorado River beaches provide a foundation for terrestrial habitat adjacent to the river as well as a safe and comfortable resting place for the recreational rafters and hikers who camp on them. In addition, sediment is important for in-place preservation of archaeological sites and other cultural resources. Most sediment entering Grand Canyon National Park now arrives from the Paria River and upper Marble Canyon tributaries below the dam.
Research is supported by pre- and post-release remote sensing to determine how the beaches and sediment in the system respond to the high flows. Aerial photography will be complemented by channel-bed mapping and sediment classification using sophisticated multibeam sonar. Subsequent remote sensing efforts around Memorial Day, 2005, and 18 months after the test will track changes in the system over time.
USGS scientists are focusing their investigations on sediment resources – specifically, how much of it moves through the Grand Canyon during the high-flow event, and how much is retained in the form of beaches or channel deposits. Shoreline beaches will be measured using a combination of conventional survey equipment and airborne Light Detection and Ranging equipment. LiDAR is a relatively new surveying technology that can deliver highly accurate topography from aircraft flying thousands of feet above the ground in remote locations. Sediment suspended in the water also will be measured using a combination of water sampling and a laser based technology.
A major portion of the research is focused on the well-being of native fish. The humpback chub, an endangered species, is one of four remaining native fish in the Grand Canyon. USGS scientists will be monitoring how the high-flow releases affect the survival of a population of young humpback chub in the Grand Canyon near the confluence of the Little Colorado River.
Non-native rainbow trout, a predatory species, are an important resource for anglers below Glen Canyon Dam in the first 15 miles, to Lees Ferry. Surveys to determine the relative abundance of trout were recently completed by the Arizona Game and Fish Department. These surveys will be repeated in mid-December, 2004, to determine the effect of the high flows on trout populations and trout diet.
Another endangered species, the Kanab ambersnail, will be the focus of an experiment to determine if its habitat can be protected from experimental floods. Vegetation occupied by snails in the zone to be inundated will be removed by hand, stacked on pallets and moved above the flood. After the high flow ends, vegetation will be relocated to the flood zone and growth hormones will be applied to plants to encourage re-establishment of snail habitat.
The aquatic foodbase is important for all species living in the river. A fundamental component of the foodbase is ”drift,” or the floating array of invertebrates, algae and other bits and pieces of raw material carried down the river as a result of the natural erosion of the channel and surrounding landscape. Drift provides a source of energy and carbon to higher organisms, including fish.
Drift samples will be taken below the Little Colorado River to determine changes in the foodbase before, during and after the high flow. Pre- and post-flood surveys of algae and aquatic vegetation beds, an important part of the foodbase, also will be conducted in the Lees Ferry reach.
Another part of an overall experiment to test the effect of flow and non-flow actions that enhance and restore natural resources in the canyon involves the removal of non-native fish from a critical habitat for the endangered humpback chub near the confluence with the Little Colorado River. While unrelated to flows, this research effort will continue in concert with the overall research design.
Scientific studies will continue after the high-flow experiment to examine the condition and status of sediment deposited on the beaches and the long-term effect on the natural and cultural resources.
For more information regarding the science associated with the experimental high flow, contact Scott Harris, public affairs officer for the U.S. Geological Survey, at (703) 648-4054 (office); or (703) 785-1113 (cell); or (877) 826-5955 (satellite phone — after Nov. 18). His e-mail is firstname.lastname@example.org.
The draft EA and Finding of No Significant Impact is at www.usbr.gov/uc/envprog/amp. The news release on the EA is at www.usbr.gov/newsroom/.