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<br />I <br /> <br />I <br /> <br />I <br /> <br />1. Estimate precipitation duration and depth for each frequency from <br />rainfall records in the area. <br />2. Arrange the total rainfall amount into a typical rainfall <br />pattern for the area. <br />3. Estimate the surface runoff deducting watershed retention and <br />losses from total precipitation. <br />4. Determine hydrograph shape using watershed characteristics. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />A similar procedure was used to prepare the spillway design hydrographs <br /> <br /> <br />for the darns, except that the probable maximum precipitation was taken <br /> <br /> <br />from Technical Paper No. 38, U.S. Weather Bureau, 1969. This publication <br /> <br /> <br />gives the probable maximum precipitation for a 6-hour duration over a 10- <br /> <br /> <br />square mile area in the region to be 22 inches. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Following completion of the Phase A part of the Little Dry Creek basin <br /> <br /> <br />study, additional preliminary design work was done on Englewood Darn by <br /> <br /> <br />the firm of Woodward-Clevenger & Associates, Inc., under contract with <br /> <br /> <br />the Urban Drainage District. Their preliminary design work was reviewed <br /> <br /> <br />as a part of the work done for this report. The spillway design hydro- <br /> <br /> <br />graph that they developed is used herein. The flood volume is about the <br /> <br /> <br />same as we calculated and reported in our Phase A Little Dry Creek study, <br /> <br /> <br />but the peak flow at Englewood Dam was 40 percent greater than our Phase <br /> <br />A calculation. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Precipitation <br /> <br />I <br /> <br />I <br /> <br />Basic rainfall data for the Little Dry Creek basin was taken from Figures <br />7-1 through 7-8 of the Drainage Criteria Manual. These figures show <br />that the depth of given frequencies of rainfall events varies substantially <br />in different parts of the basin. Accordingly, the basin was divided <br />into ei~ sub-basins and rainfall depths were calculated for each sub- <br />basin. Table 2, which follows, shows the drainage basin sub-basins together <br />with the rainfall depths for the 10, 25 and 100-year rainfall events. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />-27- <br /> <br />I <br />