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<br />I <br /> <br />I <br /> <br />I <br /> <br /> TABLE ~~ =. liUMMARY OF SPR BASIN PARAMETERS <br /> DRAINAGE AREA CURVE NUMBER TIME OF <br />SUBBASIN .umuare miles}. CN CONCENTRATION . Ie <br />A 0.50 65 0.322 <br />B 0.69 65 0.424 <br />C 0.16 67 0.348 <br />D 0.25 70 0.500 <br />E 0.20 62 0.332 <br />F 0.28 66 0.582 <br />G 0.24 69 0.457 <br />11-1 0.08 70 0.160 <br />11- 2 0.13 70 0.231 <br />J-l 0.09 79 0.271 <br />J-2 0.14 85 0.332 <br />K 0.15 82 0.470 <br />L-l 0.30 85 0.478 <br />0 0.42 74 0.686 <br /> <br />I <br /> <br />Rating curves for each of the three culverts were calculated; <br />these included weir flow for overtopping of roadways. It <br />should be noted that there is some uncertainty as to the exact <br />sizing of the Sears Shopping Center culvert. Discharge <br />estimates were based on informatIon from the ESSW and will be <br />field-verified before the hydraulic analysis is performed. <br />Approximate stage/capacity curves were obtaIned at each <br />location hy planimeter with 1:400 scale mapping at 2-foot <br />contours. <br /> <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />A stage-discharge curve for the Big Stratton Reservoir was <br />available In the ESSW report. Communication wIth the owners of <br />the reservoIr at the Myron Stratton Home indicated that normal <br />operating level of the reservoIr Is kept at an elevation well <br />below the spillway crest. However, as a conservative approach, <br />it was assumed that the reservoir was full at the beginning of <br />each storm event. <br /> <br />I <br /> <br />I <br /> <br />The peak discharge results for the 211-hour AMC II storm at the <br />locations indicated on figure 4.1 are presented in Table 4.3. <br />The 1,660 cfs value for the 100-year flood at interstate 25 is <br />approximately 9% hIgher than that established by the ESSW. <br /> <br />I <br /> <br />The difference between the two studies is primarily a <br />consequence of the difference In the two desIgn storms. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />21 <br /> <br />R€~OURC€ CON~ULTI\NT~ INC <br /> <br />I <br />