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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 />I <br />I <br />I <br /> <br />Figures 6 through 9 show runoff hydrographs for each recurrence interval for selected design <br />points under future basin development <br /> <br />Results of Hvdroloaic Analvsis <br /> <br />TABLE 5 <br /> <br />Figures 10 and 11 show discharge versus stream stationing for the 2-,5-, 10-,50- and 100-year <br />floods for the main channel of Upper Lena Gulch, Apex Gulch, and Pleasant View Tributary, <br />These plots represent peak flows for existing channel conditions under future basin <br />development <br /> <br />Location <br />Lena Gulch at Hogback <br />Lena Gulch at 6th Avenue <br />Lena Gulch at 1-70 <br />Inflow to Maple Grove Res, <br /> <br />500-YEAR PEAK DISCHARGES (cfs) <br />100-vear <br />1,770 <br />2,270 <br />3,810 <br />3,980 <br /> <br />500-vear <br />3,900 <br />4,500 <br />7,700 <br />7,800 <br /> <br />The peak discharges computed for future basin conditions are used in subsequent hydraulic <br />analyses to determine limits of flooding and the flood profile along the drainageway, <br /> <br />In addition to the analyses performed during this study to estimate peak discharges and <br />discharge hydrographs for the 10-, 50-, and 100-year frequencies, analyses were performed to <br />estimate the 500-year frequency peak discharge, <br /> <br />The 500-year frequency peak discharge was estimated by linear extrapolation of log-log plots of <br />discharge versus exceedance probability for the 2-, 5-, 10-,50-, and 100-year peak flows under <br />future basin conditions at selected design points, The estimated peak inflow to Maple Grove <br />Reservoir for the 500-year frequency event is 7,800 cfs, Table 5 shows the 500-year frequency <br />peak flows at selected design points, <br /> <br />9 <br /> <br />~ <br />