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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 />This hydrologic computation was made uSing the appropriate Area Adjustments <br />as the watershed increased in size from zero to 26.2 square miles, and <br />el iminating the hydrographs from Reference 3 representing flow from the <br />portion of the basin upstream from Interstate 25. <br /> <br />TABLE VI <br />SUMMARY OF PEAK FLOWS <br />BIG DRY CREEK <br /> <br /> Hydrologic Uncontroll ed Peak Flow <br /> Design Drainage (cfs) <br /> Point Area (sq. mil 10-yr. 100-yr. <br />Big Dry Creek at 11 ,9101 <br />168th Avenue A 65.4 5550 <br />Big Dry Creek d/s of 11 ,8101 <br />Tributary Confluence B 63.2 5520 <br />Big Dry Creek u/s of 10,6601 <br />Tributary Confluence C 55.9 5190 <br />Bi g Dry Creek at 10,8801 <br />York Street D 52.2 5320 <br />Bi g Dry Creek at 11 ,0502 <br />144th Avenue E 46.4 5490 <br />Bi g Dry Creek at 1-25 F 39.2 5640 11,1903 <br /> <br />Peak flows computed in this manner were not as large as the peak flows <br />computed from the enti re watershed storm. Thi s compari son 1 ed to the <br />conclusion that the governing hydrologic condition is a single large storm <br />occurri ng uniformly over the ent ire 65.4 square mil e watershed, wi th the <br />appropriate Area Adjustments applied. Table VI presents peak flows <br />computed in this manner. Figure 4 illustrates three typical hydrographs <br />resulting from this analysis along the Study Reach. <br /> <br />Hydraulic Analysis <br /> <br />1 <br />Peak fl ow result i ng from a des i gn storm extendi ng over the enti re <br />Uncontrolled Drainage Area tabulated. <br /> <br />A hydraulic analysis was completed along Big Dry Creek within the Study <br />Reach to determine the water surface elevations for the 10-year and the <br />100-year flood events. This hydraulic analysis was completed using the <br />HEC-2 Water Surface Profile Computer Program developed by the U.S. Army <br />Corps of Engineers (Reference 7). The peak flows (flood discharges) along <br />the Study Reach for the hydraulic analysis were obtained from the results <br />of the hydrologic study summarized in Table VI and Figure 3. <br /> <br />2 <br />Peak flow resulting from a linear interpolation between peak flows <br />at Hydrologic Design Points F and D. <br /> <br />3 Peak flow at 1-25 from Reference 3. <br /> <br />Note: All 100-year peak flows include 480 cfs base flow from Standley <br />Lake and Great Western Reservoir. <br /> <br />The computed flood profiles and limits of the 100-year floodplain are shown <br />on the Floodplain Maps (Sheets 2 through 16) and the Profiles (Sheets 17 <br />through 26). Tabulated data regarding cross sections, stationing, flood <br />elevations, and other pertinent hydraulic information are found in Table <br />VII. More detailed information regarding the hydraulic calculations is <br />available from the Urban Drainage and Flood Control District. The <br />following paragraphs describe the data collection and adjustments, and the <br />hydraulic assumptions used for the computer model in general and for <br />speCific areas within the model. <br /> <br />Cross section data for the hydraulic analysis were developed photo- <br />grammetrically by the digitizing of sections of the channel and floodplain <br /> <br />10 <br />