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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 />I <br />I <br />I <br />I <br />I <br />I <br />II <br />II <br />I <br /> <br />Table 4. Comparison of 1979 Flood Peak Estimates to TR20 Model Estimates, 100- <br />Year Event. <br /> <br /> <br />time to <br /> <br />Cl <br />C2 <br />Gl <br />G2 <br /> <br /> <br />North Clear Creek <br />100- ear time to <br />Point 1979 est. 2001 Model <br />NCI 2694 2702 <br />NC2 2528 2524 <br />NC3 2280 2267 <br />NC4 NtA 1924 <br />NC5 NtA 1311 <br />NC6 Nt A 929 <br /> <br /> <br />Note: See Figure 4 for design points. <br /> <br />IMPACT OF RESERVOIR STORAGE ON FLOOD PEAKS <br /> <br />The impact of the Chase Gulch and Dorothy Lee Reservoirs on flood peak discharges <br />was identified using the TR20 hydrologic models calibrated to reconstitute 1979 100-year <br />flood peak: estimates. Storage/elevation curves (Figures 5 and 6) were developed from <br />design and as-constructed drawings of the two reservoirs (RMC, 1991, and RMC, 1994). <br />The discharge curve for Chase Gulch Reservoir uses the spillway discharge curve <br />developed for the reservoir shown in the Appendix. The discharge curve for Dorothy Lee <br />Reservoir was calculated using the FHW A HY -8 program in the Appendix. <br /> <br />The results of the analysis for the 10-, 50-, and 100-year event are summarized at selected <br />design points on Table 5. The results for the 100-year event are found in the Appendix. <br />The results indicate detention storage above the Chase Gulch water supply reservoir <br />spillway reduces flood peaks significantly at the outlet. At the outlet. design point C I. <br />100-year discharges are reduced from 1179 cfs to 551 cfs. Dorothy Lee Reservoir has <br />only a minor impact on flood peaks during the 100-year event at the outlet of Gregory <br />Gulch. At the outlet, design point G1, 100-year discharges are reduced from 1248 cfs to <br />ll59 cfs. This reduction is less than predicted by a recent HEC-1 analysis by I.F. Sato <br />(1996), which assumed a slightly lower curve number causing a lower peak discharge <br />than the current study. In addition, the current study defined the storage and discharge <br />relationship of Dorothy Lee Reservoir using design drawings and hydraulic calculations. <br />The 1996 Sato study used simplified hydraulic relationships and did not examine the as- <br />built infollDation when modeling the reservoir. The TR20 model indicates the reservoir <br />overtops during the 100-year event <br /> <br />-10- <br />