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<br />4 <br /> <br />Jensen <br /> <br />There were 26 backwaters at the Jensen site on August 2 (table 2) with a <br />total of 10,870 m2 (flow = 1,515 ft3/s). Subsequent to fluctuating flows, <br />backwater number increased to 34, but, backwater area remained stable <br />(10,941 m2) on August 16. Stabilized flows for 6 weeks increased backwater <br />area by 36 percent to 14,930 m2 on September 28, although backwater number <br />decreased to 30. <br /> <br />Backwater area decreased by about 50 percent to 7,593 m2 on October 11, and <br />backwater numbers decreased similarly. The same concerns discussed above <br />for this date and flow apply here. <br /> <br />Ouray <br /> <br />There were 37 backwaters at the Ouray site on August 2, with a total area of <br />35,098 m2 (flow = 1,500 - 1,700 ft3/s). Following the fluctuation of flows, <br />the number of backwaters remained similar (33) while backwater area <br />decreased about 13 percent to 30,482 m2 on August 16. Subsequent to stable <br />flows for 6 weeks, backwater number increased by approximately 70 percent, <br />to 56, and backwater area also increased by 70 percent, to 51,824 m2 on <br />September 28 (flow = 1,420 ft3/s). <br /> <br />The October 11 backwater number decreased substantially, to 29, as did <br />backwater area, to 37,898 m2 (flow = about 2,500 ft3/s). The flow on this <br />date was significantly higher than on the previous dates that video was <br />collected, which probably had an impact on backwater habitat. <br /> <br />Discussion <br /> <br />It is apparent that the flows on October 11 were higher than anticipated and <br />that they had a significant, negative impact on backwater habitat. At each <br />site studied, this flow produced the fewest backwaters and the least <br />backwater area. Although these data cannot be used in the fluctuating flow <br />study, it is notable that the flow on this date (about 1,900 ft3/s) is <br />outside the range recommended by the 1987 study for optimum backwater <br />availability (Pucherelli et al., 1988), of 1,100 to 1,800 ft3/s at the <br />Jensen gauge on the Green River. <br /> <br />There are two comparisons that may be made with the remaining three video <br />events, (1) video results between August 2 and August 16, which reflect the <br />effect of daily flow fluctuations between 1,600 and 2,900 ft3/s, and <br />(2) video results between August 16 and September 28, which reflect the <br />effect of very stable daily flows. <br /> <br />Fluctuating flows of 1,600 to 2,900 ft3/s produced a substantial decrease in <br />backwater area only at the Island Park site. A smaller decrease was <br />recorded at Ouray, while backwater habitat at Jensen remained relatively <br />unchanged following this event. The decrease in backwater habitat at <br />