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<br />I <br />I, <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />The amount of rainfall and snow melt in the lower basin is small in <br />relation to the total water supply and is accounted for in this ~tudy as being <br />available to meet future agricultural uses directly. <br /> <br />Discussions with U.S. Geological Survey staff indicate that ground- <br />water flow into the lower basin is minimal and, therefore, is not included as <br />a potential future source of water supply in this study. <br /> <br />There is the possibility of additional water being available to the <br />Cache la poudre River Basin in the future from additional runoff from forest <br />management plans [4]. This has been estimated to be about 2,600 acre-feet per <br />year for that portion of the national forest lying within the basin. Since <br />this additional yield is speculative and minor in comparison to the total <br />basin yield, it was not considered as part of the future water supply during <br />this study. <br /> <br />In summary, the average annual future developable water supply at the <br />mouth of the canyon for a potential Cache la Poudre Project would consist of <br />271,000 acre-feet of native flows and 37,000 acre-feet of transbasin imports. <br />In addition, the total annual average water supply for the Cache la Poudre <br />service area would include 115,000 acre-feet of water from the combined <br />Colorado-Big Thompson Project and Windy-Gap Project, an increasing amount of <br />return flows from Fort Collins and an increasing amount of water from the Big <br />Thompson River. <br /> <br />C. INFLOlf DESIGN FLOODS <br /> <br />I <br />I <br />J <br /> <br />The inflow design floods for potential dams considered as part of this <br />study were determined from an envelope curve of flood peak versus drainage <br />area which is shown in Figure 111-7. The curve was determined from the record <br />of all measured major flood peaks along the front range and piedmont in <br />Colorado and some inflow design flood values developed for existing reservoirs <br />in the Cache la poudre area. <br /> <br />I <br /> <br />By inspecting the information in Figure III-7, an. envelope curve with a <br />Creager's C 'of 150 was chosen for preliminary planning of all potential dam- <br />sites except for the New Seaman Dam and inflow design flood peaks which were <br />estimated based on the area above the potential damsite. (The inflow design <br />flood for New Seaman Dam was developed during recent studies by International <br />Engineering Company [28]). The resulting values were used in sizing and <br />estimating costs of spillways for the potential dams. The difference in the <br />cost of the spillways designed to carry different peak flood discharges <br />(obtained by using different values of C) was determined to be minimal when <br />considering the accuracy of designs and cost estimates at the level of detail <br />being employed in this study. <br /> <br />I <br /> <br />I <br />I <br />I <br /> <br />The inflow design floods for the major reservoirs considered in the study <br />are as follows: <br /> <br />III-5 <br /> <br />I <br />