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Lower South Platte River Study <br /> Colorado Water Conservation Board <br /> December 2001 <br /> February 1954 to April 1957 (1950s Drought) <br /> ' February 1976 to November 1980 (1970s Drought) <br /> In most years, water is consistently available in December and January with some water <br /> available in the February to mid-April period. However, some extremely large volumes of <br /> water are available in isolated years in the months of May and June. For example, the <br /> analysis indicates that nearly 692,000 acre-feet would have been available in the river at the <br /> ' North Sterling Inlet Canal diversion in June 1983 and nearly 539,000 acre-feet in June 1995. <br /> These were two extremely wet years. <br /> Because of the extreme variability of the available water supply estimates, the development <br /> of a dependable water supply will require storage. <br /> ' 2.5 Storage Analyses <br /> 9 Y <br /> ' A simplified spreadsheet operations model was developed by Brown and Caldwell to <br /> evaluate potential storage options. The model covers diversions of water at the: <br /> • North Sterling Canal Headgate <br /> • Harmony Ditch Headgate <br /> ' • Peterson Ditch Headgate <br /> ' The canal systems supplied by these diversions could be used to fill storage in a new <br /> reservoir by gravity or by pumping, depending on the availability of delivery capacity after <br /> current water users on the canal are satisfied. <br /> ' As discussed in Section 2.4, water is consistently available in the river during the winter <br /> months. However, the river headgates and the canals and ditches are very difficult to operate <br /> ' and maintain during the winter due to ice conditions. The only canal that is operated <br /> successfully in winter is the North Sterling Inlet Canal, which is a deep v-shaped channel <br /> ' with few structures. Because of its length (>100 miles), configuration, and number of <br /> crossing and turnout structures, the North Sterling system appears to be the least attractive <br /> option for filling a new storage reservoir by gravity. Water to fill new storage would be <br /> ' diverted at the North Sterling Inlet, travel 50 miles to North Sterling Reservoir and another <br /> 60 miles to storage sites west of Julesburg Reservoir. <br /> ' The Harmony system is better suited to this type of operation,but is located at elevations <br /> lower than many of the storage sites that were identified upstream of Julesburg Reservoir. <br /> The Harmony system could be used to fill an enlarged Julesburg Reservoir and sites on the <br /> ' north side of the river downstream of Julesburg Reservoir by gravity. Water could be <br /> pumped from the Harmony system into the storage sites topographically higher than the <br /> ditch. <br /> GEI Consultants, Inc. 2-9 01002 Dec 2001 Lower South Platte River Study <br />