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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 />F L 0 0 D <br /> <br />S TAG E <br /> <br />D E T E R M I N A T ION <br /> <br />Flood stages were determined along Little Dry Creek and its major tribu- <br /> <br /> <br />taries for several different conditions. Flood stage determinations were <br /> <br /> <br />made for both present and estimated ultimate future condition of urbani- <br /> <br /> <br />zation in the basin in order to make the information useful for planning <br /> <br /> <br />future drainage works and enforcing land use regulations. By comparing <br /> <br /> <br />Tables 5 and 6 it will be seen that flood peaks and volumes under esti- <br /> <br /> <br />mated future conditions are only slightly greater than those to be ex- <br /> <br /> <br />pected under present conditions. <br /> <br />Flood stages were computed for 10, 25, and lOa-year frequency floods in <br /> <br /> <br />order to develop flood damage estimates. Flood stages were also computed <br /> <br /> <br />for three degrees of flood detention dam development: (1) with no dams, <br /> <br /> <br />(2) with Englewood Dam only, and (3) with Englewood Dam plus the five pro- <br /> <br /> <br />posed additional detention dams. The six detention dam development results <br /> <br /> <br />in the greatest reduction in flood peaks in the Little Dry Creek Basin. <br /> <br />Flood water levels were computed by conventional open channel hydraulic <br /> <br /> <br />analysis methods. Channel roughness characteristics were determined by <br /> <br /> <br />a field inspection of the waterways in May 1972. These roughness factors <br /> <br /> <br />were increased slightly to reflect the greater growth of vegetation that <br /> <br /> <br />could be expected in the summer months. It is estimated that natural chan- <br /> <br /> <br />nel roughness will not increase significantly in the future as a result of <br /> <br /> <br />vegetal growth, although the construction of fences and buildings in the <br /> <br /> <br />flood plains would impede flow and cause flood levels to rise. <br /> <br />Water levels were calculated at waterway cross sections that were normally <br /> <br /> <br />300 to 500 feet apart. In a few cases sections were 600 to 700 feet apart. <br /> <br /> <br />Where abrupt channel constrictions occurred, cross section spacing as close <br /> <br /> <br />as 10 feet was used. A major part of the water level calculations were done <br /> <br /> <br />using an IBM 370 computer. The computer program used was a Reclamation <br /> <br />-46- <br />