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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 />Hydrograph shape depends on a number of watershed characteristics, The configuration <br /> <br />of the watershed and its slope are two of the most important characteristics, A short, wide <br /> <br />watershed can be expected to have a high rate of peak discharge that develops quickly, while <br /> <br />~ <br />P-;U] <br /><1lZ <br />aQ;;:O <br />Zt.'JH <br />HOE-< <br />ZAO <br />3~~ <br />O-i~Cl <br />~ <br />~~~ <br /><JlU~ <br />~ZE-< <br />~O~ <br />c.!l_~ <br />-<E-l <br />ZZ~ <br />~~0 <br />~I's'lZ <br />AAH <br />~~~ <br />O~H <br />HH:x:1 <br />~~~ <br />c.!l-<~ <br />z:>-< <br />oZ~ <br />oo?-i <br />~E-<O <br />r.lJ.O <br />~.-i <br />~ <br /> <br />a long, narrow watershed will have a relatively lower peak discharge that develops more <br /> <br />slowly. A steeply sloped watershed will have a relatively higher peak rate of discharge that <br /> <br />develops more quickly than would a more gently sloping watershed. Peak rates from <br /> <br />upstream water shed areas may be reduced as they pass through long, narrow, gently sloping <br /> <br />watersheds because of the effect of natural channel and flood plain storage capacity. A <br /> <br />synthetic unit hydrograph method was used to develop flood hydrographs for the Moon <br /> <br />Gulch basins. The unit hydrograph method used is the Colorado Urban Hydrograph <br /> <br />Procedure as described in the Drainage Criteria Manual. In this method, it is first necessary <br /> <br />to determine the area, stream length, location of the centroid, and the average slope of each <br /> <br />sub-basin drainage area. These physical characteristics of each sub-basin plus two empirical <br /> <br />coefficients were used to develop the unit hydro graphs. The empirical coefficients, Ct and <br /> <br />Cp' are coefficients of time to unit hydrograph peak and peak rate of runoff, respectively. <br /> <br /> <br />These coefficients are given in the Drainage Criteria Manual for 60, 40 and 20 percent of <br /> <br />watershed imperviousness, and it was necessary to interpolate to obtain coefficients for the <br /> <br />estimated percent imperviousness for future land use conditions of the basins. <br /> <br />Figure 3- shows the 100-year hydrographs for existing and-future basin development at the <br /> <br />Ralston Valley Detention Cell at 72nd Avenue and Eldridge Street. <br /> <br />The projected peak discharges along the Moon Gulch channel are shown in Figure 4. <br /> <br />-12- <br /> <br /> ~ <br /> t3 <br /> t- <br /> ~ <br /> .Y <br /> ~ ~ <br /> ~ ~ <br /> ./ <br /> ~ P r' <br /> ~ ,J <br /> ,..../ <br />( ~ (: <br /> ; <br /> '\ <br /> - I , <br /> \..J , <br /> ~ <br /> - <br /> <br /> - <br />0 0 0 0 0 0 0 0 0 0 <br />0 0 0 0 0 0 0 0 0 0 <br />0 f'- ..q- ..- CO l[) N <>> to to <br />t'l 0J 0J ('\J ~ ~ ~ <br /> (So!!::)) M.O'I.!l <br /> -13- <br /> <br />o <br />o <br /> <br />o <br />l[} <br />N <br /> <br />t{) <br />N <br />0J <br /> <br />o <br />o <br />N <br /> <br /> W <br /> 0::: <br /> :=) <br /> f- <br /> :=) <br /> LL <br /> 0::: <br /> <( <br /> W <br /> >- <br />-- 0 <br />[Ii <br />r:q 0 <br />E-< ..-- <br />~ 0 <br />Z <br />- <br />~ () <br />-- Z <br />ri:l f- <br />~ (f) <br />H X <br />E-4 W <br /> 0::: <br /> <( <br /> w <br /> >- <br /> 0 <br /> 0 <br /> ..-- <br /> + <br /> <br />l[) <br />l' <br /> <br />..-- <br /> <br />o <br />l[} <br /> <br />..-- <br /> <br />l[} <br />N <br /> <br />..-- <br /> <br />o <br />o <br /> <br />..-- <br /> <br />II) <br />f'-.o <br /> <br />o <br />L!) <br /> <br />II) <br />N <br /> <br />'" <br />w <br />'" <br />=> <br /><> <br />u: <br />