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<br />productivity during base flow period (i.e., cover 95% of the surface area), flows of 400-500 cfs <br /> <br /> <br />are needed; and ifflows fall below 161 cfs, riffle habitat declines rapidly. However, between 1923 <br /> <br /> <br />and 1997 baseflow (August through October) discharge in the White River (Watson gage) has <br /> <br /> <br />only dropped below 200 cfs less than 5% of the time. Further, baseflow discharge on the White <br /> <br /> <br />River (Watson gage) has been below 150 cfs less than 1 % of the time. <br /> <br /> <br />Finally, we point out that under the current flow regime (the past 20 years), the Colorado <br /> <br /> <br />pikeminnow population has done well in the White River. Preliminary population estimates <br /> <br /> <br />suggest that the density in the White River are two or three times the density in the Yampa River <br /> <br /> <br />(Bestgen et al. 2002), and Interagency Standardized Monitoring Program suggests that Colorado <br /> <br /> <br />pikeminnow numbers have increased in recent years (1986-2000) and that the White River has <br /> <br /> <br />increased most of all (McAda 2002). Irving and Modde (1994) suggested that Taylor Draw Dam <br /> <br /> <br />may concentrate fish by preventing upstream movement and may have increased the prey base <br /> <br /> <br />downstream and artificially increased carrying capacity for large predators such as Colorado <br /> <br /> <br />pikeminnow. Or perhaps the relatively large base flows, at least compared to the near by <br /> <br />Duchesne River, may attract more fish. Unfortunately, w~ do not yet know why it attracts so <br /> <br />many Colorado pikeminnow. <br /> <br />CONCLUSIONS <br /> <br />1. There is a great deal of uncertainty in the precision, interpretation, and scope of this study, but <br /> <br />listed below are the results we found. <br /> <br />19 <br />