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<br />two principal areas; the lower reaches of the Yampa River and in Desolation/Gray Canyon of the <br />Green River (Tyus and Haines 1991). Newly-hatched larvae from the Yampa River drift to principal <br />nursery backwaters between Split Mountain (River Kilometer [RK] 513; i.e., distance upstream from <br />the confluence of the Green and Colorado rivers) and Sand Wash (RK 346), and larvae from <br />Desolation/Gray Canyon drift to backwaters between Green River (RK 191) and the Colorado River <br />contluence (RK 0; Tyus 1991). The densities of these young fish are often high in fall, but decrease <br />by an average of 46-54% by spring (Haines and Modde 1996; Valdez and Cowdell1996; McAda and <br />Rye! 1999; Valdez et a1. 1999), indicating substantial overwinter mortality, which we believe is <br />abnormally high and contributes to reduced recruitment and continued endangerment of the species. <br />The causes for these decreased densities are unknown, but may be related to unstable nursery <br />backwaters from fluctuating dam releases; infringement of backwaters by ice processes; predation <br />by non-native fishes; natural downstream dispersal by young Colorado pikeminnow, which ar~ <br />potomadromous or long-distance migrators as adults (Tyus 1984); and condition or fat content of <br />the young fish at the beginning of winter (Thompson et al. 1991). <br /> <br />Purpose and Objectives <br /> <br />The purpose of this study was to determine the effect of winter flow regulation from Flaming <br />Gorge Dam on ice development and breakup on the Green River and the effect of these ice processes <br />on nursery habitat of age-O Colorado pikeminnow. We hypothesized that the current pattern of ice <br />development and breakup on the Green River downstream of Flaming Gorge Dam are linked to dam <br />operations, and that these ice processes significantly reduce availability and persistence of backwater <br />habitat for overwintering age-O Colorado pikeminnow in one of the primary nursery areas on the <br />Green River. <br /> <br />The objectives of the study were to: <br /> <br />1. Determine if there is a link between dam operations and ice development and <br />breakup in the nursery area of Colorado pikeminnow, <br /> <br />2. Determine availability of overwinter nursery backwater habitat for age-O Colorado <br />pikeminnow, <br /> <br />3. Determine condition and longevity of backwaters exposed to winter flow regulation <br />and ice development and breakup, and <br /> <br />4. Recommend winter releases from Flaming Gorge Dam to protect nursery habitat of <br />age-O Colorado pikeminnow. <br /> <br />STUDY AREA <br /> <br />The study was conducted on the upper Green River in eastern Utah, downstream from <br />Flaming Gorge Dam (Figure 1). The dam is at an elevation of 1,708 m about 658 km upstream from <br />the confluence with the Colorado River. The study area extended from Island Park (RK536), within <br /> <br />3 <br />