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Last modified
7/14/2009 5:02:31 PM
Creation date
5/20/2009 3:40:19 PM
Metadata
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UCREFRP
UCREFRP Catalog Number
7820
Author
Rakowski, C. L., J. C. Schmidt and T. A. Crowl.
Title
Geomorphic Response of a Sand-Bed River to High Discharge; Effects on Colorado Squawfish Nursery Habitat Availability, (poster presented at 1993 Fall Meeting of American Geophysical Union).
USFW Year
1994.
USFW - Doc Type
\
Copyright Material
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<br />INTRODUCTION <br /> <br />""~ <br /> <br />The study site is located on the Green River, within the Ouray National Wildlife Refuge. <br />About 50 percent of river flow at the study site is controlled by water releases from Flaming Gorge <br />Dam; the remainder of the streamflow originates from the unregulated Yampa River. <br />Colorado squawfish (Ptychocheilus lucius) are endemic to the Colorado River basin and were <br />once abundant. The fish was included in the original list of endangered species by the US Fish and <br />Wildlife Service in 1967. Squawfish spawn on cobble and gravel substrate on the lower Yampa <br />River on the descending limb of the spring snowmelt hydrograph. Larval fish emerge after an <br />incubation time of about I week and are transported or move downstream. Larval fish occupy <br />stagnant flow habitats associated with emergent sand bars in the Ouray reach (Fig. 1) (Tyus, 1990). <br />These fish remain in these sites throughout the summer and fall. One objective of water release <br />management of Flaming Gorge Dam is to maximize the available areas of stagnant water and eddies <br />(backwaters) to maximize and maintain nursery habitat availability. <br /> <br />Research Objectives <br /> <br />. Characterize the geomorphology of Colorado squawfish nursery habitat <br />. Determine if different geomorphic settings give rise to nursery habitats of different <br />qualities <br />. Develop flow recommendations for formation and maintenance of high quality nursery <br />habitat. <br /> <br />1993 Field Season Objectives <br /> <br />1 Characterize the geomorphology of the reach. <br />2 Quantify the extent and magnitude of bed response to the passage of a "normal" flood, <br />occurring after a seven-year drought period. <br />3 Measure changes in channel cross sections on the descending limb and during low flow <br />regimes. Establish a data set to further calibrate the bed behavior model of Andrews and <br />Nelson (1989). <br />4 Relate bar changes to changes in available Colorado Squawfish nursery habitat. <br /> <br />STUDY SITE <br /> <br />The Green River near Ouray is characterized by alternate and mid-channel bars that have <br />largely remained fixed during the past 30 years. Reduced flood peaks have caused channel <br />simplification (e.g. filling of some secondary channels), although there have also been many areas <br />of bank erosion. <br />The study reach was established by Andrews and Nelson (1989), who applied a numerical <br />flow and bed behavior model to this reach. Their cross-sections were replicated by the U.S. Fish and <br />Wildlife Service and Bureau of Reclamation (1. Lyons, G. Smith, written comm.) in 1987 and 1990. <br />We reoccupied this site in fall 1992. <br /> <br />The intensive study site is 1.3 km in length (Fig. 2), and is located within a 16-km reach <br />
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