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<br />. <br /> <br />DRAfT <br /> <br />. <br /> <br />behavior. During periods of low flow in year 1, more backwater habi tat became <br />available and correspondingly more squawfish were found in backwaters <br />indicating that the foraging squawfish were attracted to these areas by <br />concentrations of small fishes. Use of ice-covered backwaters during both <br />years indicates that the fish were both foraging and resting in this habitat. <br /> <br />6.2.2 Razorback Sucker <br /> <br />. <br /> <br />During the first year of the investigation, 8 radiotagged razorback suckers <br />were observed in only two habitat types; runs and eddies. The fish spent <br />approximately 64 and 31% of the time in these habitats, respectively (Figure <br />17A) . <br /> <br />. <br /> <br />During year 2, the 10 razorbacks observed during ice-free conditions used runs, <br />eddies and slackwaters approximately 48, 30, and 22% of the time, respectively <br />(Figure 17B). Use of the term slackwater is explained in the section above for <br />Colorado squawfish. These fish used runs (89%) almost exclusively during <br />iced conditions in year 2, although some habitats were probably slackwaters but <br />could not be distinguished because of the ice cover (Figure 17C). <br /> <br />. <br /> <br />Like the Colorado squawfish, razorback suckers used winter habitats that were <br />characteristically of moderate depth and low velocity. Their selection for <br />these habitats also seemed to be driven by low near-bottom velocity. However, <br />unlike squawfish, razorbacks did not appear to use ice as a cover element. <br />Their use of depth, velocity and substrate is explained in detail in the <br />section on HSI CUrve Development. <br /> <br />. <br /> <br />6. 3 RES~SE OF HABITATS AND RADIOTAGGED FISH TO TEST FI..CMS <br /> <br />. <br /> <br />Flows requested by BIO;WEST and provided by BOR proved very valuable in <br />observing the effect of sudden and dramatic changes in flow stage on the <br />habitat and the fish. This information may be the most important in assessing <br />flow needs by the fish. These test flows were provided three times during the <br />study and will be described more fully in later drafts of this report. For <br />now, a description is provided of the test flows observed on January 7, 1988 at <br />Rainbow Park. <br /> <br />. <br /> <br />Test flows were released from Flaming Gorge on January 6, 1988, and observed in <br />Rainbow Park on the morning of January 7, 1988. Flows were raised from 800 cfs <br />to 4000 cfs starting at 7:00 am and maintained until 8:00 pm on January 6. A <br />realized low flow of 1500 cfs was predicted to reach Rainbow Park at 9:00 am <br />and steadily increase to a high of 3900 cfs at 5:00 pm. Two crews monitored a <br />total of three fish (two Colorado squawfish, OR-3235, OR- 3236; and one <br />razorback sucker, OR-3234) during the 10-hour daytime observation period of <br />8:00 am to 6:00 pm, recording fish movement and relative water level. <br /> <br />. <br /> <br />. <br /> <br />Inclement weather and very hazardous riverine ice conditions impeded the crews <br />from contacting the fish very early on January 7. Nevertheless, a semi- <br />permanent staff gauge was established near the fish and monitored starting at <br />8:56 am (a hole had to be drilled through the ice and water level monitored in <br />the hole). Relative water level readings were recorded periodically until 4:50 <br />pm. A minimum relative water level (RWL) of 422 rom was recorded on the first <br /> <br />34 <br /> <br />. <br />