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<br />12 <br /> <br />Preferred Habitat of Rare Fishes <br /> <br />Physical Components <br /> <br /> <br />River temperature varied considerably on a diel basis during this <br /> <br /> <br />study (Figure 2). Early morning temperatures were generally 3 to 5 C <br /> <br />cooler than late afternoon levels. Backwaters were the warmest areas, <br /> <br /> <br />often warming 3-8 degrees above that of the river proper in late after- <br /> <br />noon. Morning temperatures in the Jensen area in August were usually <br /> <br /> <br />15-17 C (River Mile 178). Morning temperatures in August in downstream <br /> <br /> <br />areas varied considerably with local weather conditions, but were gener- <br /> <br />ally warmer (19-21 C) than those at Jensen. September temperatures in <br /> <br />Desolation Canyon (River Mile 30) were much colder (a low of 10.5 C) <br /> <br /> <br />due to the cool ambient air. <br /> <br />The level of the Green River in the study area fluctuates daily due <br /> <br /> <br />to releases from Flaming Gorge Dam. The greatest fluctuation occurred <br /> <br /> <br />at Jensen where a l6-inch daily rise and fall was noted. Diel fluctua- <br /> <br />tions in Desolation Canyon were only 3 to 4 inches. The large fluctua- <br /> <br /> <br />tion noted at Jensen caused a considerable daily change in available <br /> <br />habitat. Low flows provided a variety of habitat types, especially back- <br /> <br /> <br />waters. High flows reduced the number of backwaters and generally cre- <br /> <br />ated a full channel situation (i.e., wetted area unbroken by sand bars, <br /> <br /> <br />etc.). In this area, juvenile squawfish were primarily caught either <br /> <br /> <br />during low river levels when backwaters were available, or in backwaters <br /> <br /> <br />which were not affected by the fluctuations. <br />