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normal 24-hour releases usually ranged between 600 and 800 cfs, producing stage changes in the nursery <br />area of <0.1 m at the upper end and <0.01 m and the lower end. These fluctuations did not alter physical <br />morphology of backwaters studied in the Ouray Backwater Complex. These stage changes had only <br />minimal affect on backwater habitats and were limited to the upper end of the nursery area. <br />In contrast to flow fluctuations, the formation of ice jams, as observed in the 1999-2000 winter, <br />had far greater affect on backwater nurseryhabitats. Ice jams increased stage by 0.75-1.50 m, and <br />transformed many backwater habitats into flow-through areas. In association with backwater <br />transformation to flow-through environments, fish may be flushed into the surrounding system and incur <br />increased risk of injury, predation, and metabolic cost associated with the search for another suitable <br />nursery area (Haines et al. 1998; Muth et al. 2000). The role of fluctuating winter flows from Flaming <br />Gorge in the creation of ice jams is unclear to us. Valdez and Cowdell (1999) speculated that fluctuating <br />winter flows dismantle ice cover which facilitates the formation of frazil ice, and potentially results in ice <br />jams that increase river stage several meters thus inundating many backwaters. However, Hayse et al. <br />(2000) found that fluctuating winter flows did not dismantle ice cover or promote formation of frazil ice <br />and ice jams. Whatever the cause, it is likely that ice jams format several locations on the middle Green <br />River nursery area in most years (Valdez and Cowdell 1999; Hayes et al. 2000). <br />Winter Sampling for Age-0 Colorado pikeminnow <br />Prior to ice formation, the most effective method for catching age-0 Colorado pikeminnow was <br />seining. Seining was most effective when backwaters were warm and became less efficient as <br />temperatures cooled. Colorado pikeminnow that occupied backwaters on the first pass during autumn <br />sampling often vacated them prior to subsequent passes, especially when slush ice was found in the <br />backwaters. During ice cover, all gear types were ineffective for capturing age-0 Colorado pikeminnow. <br />Over the three year study period, only one young-of-year Colorado pikeminnow was captured under ice <br />xiii