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Fluctuating winter flows with icy conditions may cause movement of <br />overwintering adults, and this presumably causes stress. Stable flows are <br />recommended. <br />Recommendations <br />Flow and Temperature <br />Decline and endangerment of the Colorado River fishes is due in part, to <br />human-induced habitat changes. Closure and operation of Flaming Gorge and <br />Fontenelle dams on the upper Green River eliminated most of the native fishes <br />in 128 km of river above DNM (Baxter and Simon 1970, Vanicek et al. 1970) and <br />current operations do not provide desirable flow and temperature conditions <br />for downstream native fish populations. Standing crops of endangered fishes in <br />the Green River below its confluence with the Yampa River are presumably being <br />maintained by the more natural flow and temperature regimens of that system <br />(Tyus and Karp 1989). Reproduction of Colorado squawfish in the lower Green <br />River continues because of mitigating affects of tributary flows and increased <br />distance from Flaming Gorge Dam. <br />Miller et al. (1982c) provided some flow recommendations for Colorado <br />squawfish in the Green River which considered survival, rather than <br />maintenance or recovery, of self-sustaining populations. These investigators <br />recognized that additional flows were needed to maintain endangered fish <br />habitat, but could not identify them because of limited information. Operation <br />of Flaming Gorge Dam can be altered to aid recovery of the endangered <br />Colorado River fishes. Efforts to coordinate timing of key Green (via <br />operation of Flaming Gorge Dam) and Yampa river flow events should be <br />explored for recovery of the rare fishes in the Green River basin. <br />Acceptable flows and temperatures will require two major changes in <br />Flaming Gorge operations: higher and warmer spring releases, and lower, more <br />stable flows during the remainder of the year. Recommended flow regimes, by <br />season are: <br />SPring (March 21-June 21) <br />Flaming Gorge releases should pattern spring flows of the Yampa River, <br />particularly with respect to timing and duration. Maximum streamflow of 113.2 <br />m /s or more of warmest available water (highest lake levels) should be <br />provided annually. These releases should be synchronized with Yampa River <br />spring runoff, and occur for a period o~ about three to six weeks, resulting <br />in an average flow in excess of 367.9 m /s at Ouray, ~tah (sum of average peak <br />flow at mouth of Yampa River, 254.7 m3/s, and 113.2 m /s released fr~m Flaming <br />Gorge Dam). This flow should be followed by flows of at least 56.6 m /s for an <br />additional week. Bottomlands in the Jensen and Ouray areas would thereby be <br />flooded but fish access may need improvement. Water temperatures during <br />Colorado squawfish migrations should range from 14°C or more on May 23 to <br />about 22°C on July 27. Water temperature should reach 20°C by June 1. <br />Summer (June 22-September 22) <br />Green River flows should decrease gradually in concert with the emergence <br />of larval Colorado squawfish on spawning grounds in Yampa and Desolation-Gray <br />canyons. The flow regimen of the Green River should resemble (in timing, <br />duration) the hydrologic conditions of the Yampa River with respect to low, <br />moderate, and high water flows. Gradual decreases in spring flows sho~ld be <br />initiated with larval drift, attaining a target flow of about 50.94 m /s at <br />28 <br />