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<br />for all White River flows. This was because Yampa River fish used depths> 1.2 m and these were <br /> <br />relatively rare in the White River. And finally, a fourth curve was the maximum WUA score <br /> <br /> <br />possible, i.e., the total surface area available. It showed that suitable habitat for Colorado <br /> <br /> <br />pikeminnow was less than half the total surface area available. <br /> <br /> <br />Fish Passage <br />Table 6 summarizes the thalweg (i.e.,maximum) depth at each riffle cross section at flows <br /> <br />between 100 and 300 cfs. A discharge of300 cfs produced thalweg depths >30 cm for 47 of 49 <br /> <br />riffle cross sections, and the two that did not had a depth of 27 cm. At 250 cfs, 46 thalweg depths <br /> <br />were >30 cm; at 200 cfs, 45; at 150 cfs, 45; and at 100 cfs, 45 had depths> 30 cm. One of the <br /> <br /> <br />shallowest riffles was located just below Taylor Draw Dam at RM 104.4, the other shallow riffles <br /> <br />were all between RM 20 and 48. <br /> <br /> <br />Frequency of Low Flows <br /> <br />The historic hydrograph (1979-1996) showed that mean base flow (August through <br /> <br />October) discharge ranged from 272 to 939 cfs. The 500,10 exceedance discharge for August <br /> <br /> <br />through October was 399 cfs. A discharge of 150 cfs during the same period had an exceedance <br /> <br />value of about 95% (Figure 11). White River discharge during the base flow period 1923 to 1997 <br /> <br />had dropped below 200 cfs less than 5% of the time and below 150 cfs less than 1 % of the time. <br /> <br />DISCUSSION <br />This study took two approaches for identifYing a base flow that would protect the needs <br /> <br />of adult Colorado pikeminnow in the White River, protection of resting and foraging habitats and <br /> <br />protection of riffle habitat to maintain biological productivity that supports the Colorado <br /> <br />12 <br />