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<br />V-IO <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br /> <br />Minimum streamflows of 120 cfs on the North Fork and 200 cfs on the mainstem <br />to the confluence with Piceance Creek were provided, if possible. Meeting <br />120 cfs or the historic minimum flow in the North Fork presented no <br />operational difficulty except in the extremely dry winter months of 1977-78, <br />during which nine months of historic flow were below 120 cfs. During that <br />period of the study, six months of 90 cfs instream flows were imposed some <br />10 to 20 cfs below historic flows. Inspection o~ the full study period <br />showed that only in years in which the June reservoir level was less than <br />40,000 acre-feet would such a reduction below the historic flows be <br />necessary in the following winter months. In all other cases, carryover <br />storage was sufficient to maintain the minimum flows. <br /> <br />Minimum streamflows of 200 cfs were provided below the junction of the North <br />and South Forks. This flow was present in the stream down to the confluence <br />with Sheep Creek during all summer months. At Sheep Creek, water was <br />diverted to Piceance Creek for use in the oil shale industry. Below that <br />diversion, the flows fell below 200 cfs a number of times, but were reduced <br />below 150 cfs in only six months. Four of those months were in the extrem~ <br />dry year of 1977. <br /> <br />The operation of Avery and Sawmill Mountain Reservoirs is also affected by <br />the size of the diversion works and intake pipeline. For economic reasons, <br />it is desirable to use the smallest intake which will satisfy the storage <br />requirements. An analysis was made of the relationships of monthly capacity <br />for storage to the divertible flow in the North Fork at the decreed <br />diversion points. It was found that the streamflows on the North ForI< <br />exceeded a divertible flow of 250 cfs in only eight out of the 324 months in <br />the study period. Since the monthly flows do not reflect daily peaks, it <br />was decided to use this flow rate for intake design. Future analysis of <br />daily flows, which was beyond the scope of this study, may result in some <br />reduction of intake capacity with a corresponding decrease in costs. <br /> <br />The results of the operation studies for lIvery and Sawmi 11 Mountain sites <br />are almost identical because of the proximity of the reservoir sites and <br />corresponding diversion points. Figure V-3 illustrates the fluctuations of <br />