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once again available to the population. This will require a combination of <br />higher spring flows and management of the Grand Valley floodplain. The <br />leasing or purchase of key riverfront areas in the Grand Valley where <br />dikes could be removed and the adjacent low-lying lands allowed to flood <br />should be explored. Natural draining of such areas after runoff would <br />prevent the establishment of resident populations of predacious fish. <br />Recommendations <br />Analyses of data collected in the Grand Valley (Osmundson and Kaeding <br />1989, and new data presented here) and in downstream reaches of the Colo- <br />rado River (McAda and Kaeding 1989) have revealed a strong relationship <br />between flows and the annual abundance of Colorado squaFfish young. The <br />high-flow years of 1983 and 1984 resulted in low catch rates of young <br />Colorado squawfish, as did the low-water years of 1988 and 1989. Peak <br />flows during 1983 and 1984 at the State line gage were 60,200 and 68,300 <br />cfs, respectively; during 1988 and 1989, peak flows there were 15,000 and <br />9,480 cfs, respectively. Based on data currently available, we feel that <br />flow conditions of 1985 should be viewed as optimal for maximum production <br />of Colorado squawfish young, followed by those of 1986. It is not known <br />whether flows somewhat higher than those provided during these years, but <br />not as high as 1983 and 1984 levels, would result in even greater produc- <br />tion of young. It is also possible that physical as well as biotic changes <br />brought about by the high flows of 1983 and 1984 provided the necessary <br />conditions that were conducive to the relatively high reproductive success <br />realized in the succeeding two years. Flow conditions and production of <br />young should never fall below 1987 levels (State line peak of 22,000 cfs); <br />except during years of extreme drought, such flows should be viewed as the <br />J <br />minimum acceptable. <br />J <br />42