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<br />" <br /> <br />.::1: <br /> <br />-f - <br />. ----- --~ <br />,-.- ..._- <br />----. ----., <br /> <br />'" <br /> <br />::".--t <br /> <br />..., <br />,... <br /> <br />, <br />1 <br />,- <br /> <br />- -,., <br />__.n_, <br /> <br />- 'r. , <br />........ '1 <br />---!-'--. <br />-.--.. <br /> <br />" <br /> <br />-'-.f - <br />-~ -.... <br />n, _.. <br />--~. -.--. <br /> <br />1..-. ._ <br />'t-------- <br /> <br />.--_4 <br /> <br />" <br /> <br /> <br />-.-..-.-- <br />'r_ <br />--._- <br /> <br />.__"::..:u_:;_=--_ <br /> <br />- E- <br />- . <br />--"'r :~ <br /> <br />. ---I-- <br /> <br />..._- <br /> <br />-,,",,,,,,,-. <br /> <br />, <br /> <br />,._~_._- <br /> <br />,-:,.....-.-.,-.,", <br /> <br />~,.,--,<-:~ <br /> <br />- <br />" . <br />, <br />o <br />~ , <br /> <br />;~" , <br /> <br />.-,-=. <br /> <br />" <br /> <br />-.- .."~-'~;;, <br /> <br />- <br /> <br />z <br />" . <br />~ <br />~ <br />~ <br />~ <br />c <br /> <br />.- ----- <br />.-_.0.......... <br />- ..- <br /> <br />, <br /> <br />, <br /> <br />, <br /> <br />Co " 'r' ""'. <br />@' '--:..,:~._. <br />. . -..." <br />~_.._.._._.- <br />-- -. --.-- <br />. . . <br />~ ..... -_.~.. <br />, <br /> <br />, <br />, <br /> <br />r <br /> <br />-1-' . <br />...- <br />--1. <br />i. <br />, <br /> <br />, <br /> <br />, <br /> <br />, <br /> <br />PRECiPITATION (inches] <br /> <br />-l <br />-+~ <br />I '-.:-j <br /> <br />Detailed computations for various floods on the Sand Creek water- <br />are presented in the Technical Addendum (Leaf, 1933). <br />Design hydrographs for Sand Creek at Pioneer Park for 5,10,25,50, <br />lOO, and 500-yearfloods aresl10wn in Figure 10. Table 1 sUlll11arizes <br />design peak flows and runoff volumes generated from a 3-hour storm. <br />Regional Design Curves <br /> <br />S.3. <br />sheds <br /> <br />Undeveloped Areas <br />From the analysis aT peaK flews for the 5 through SOO-year floods <br />on Sand CreeK, 5-1, 5-2, and 5-3, a series of relationships were developed <br />which relate flood peaKs for a given recurrence interval to basin drainage <br />area. These relationships, plotted in Figurel1,wereused to estimate <br />flood peaKs on the undeveloped portions of watersheds comprising the <br />remainder of the drainage baSin tributary to the Pioneer Ditch (Figure 8). <br />As seen in Figure 8 the remaining drainage uea lies generally below <br />Sterling NO.1 Ditch between Riverside Cemetary and the east-west segment <br />of the Pioneer Ditch. <br /> <br />Developed Areas <br />PeaK Flows in thePioneerOitchgeneratedbythedevelopedportlon of <br />the drainage basin were estimated using the.'Rational equation" written <br />as: <br /> <br />-~:~ <br /> <br />Q "'CIA <br />where Q '" the peak flow in c.f.s., <br />C : the runoff coefficient, <br />I . the rainfall intensity corresponding to the time of <br />concent:-ationof the watershed in in./hr., and <br />A '" the watershed area in acres. <br />Runoff coefficients were determined from an anlysis of impervious areas <br />within the city limits of Sterling. Average impervious area varies from <br />24 to 80 ~"rc"nt in " se<,;tors of the city. As.url~<.i runuff <,;ol!f1ciel,t, <br />for each sector are as follows: <br /> <br />-0 <br /> <br />LJ <br />. I <br />I . , <br />, <br />I <br /> <br />Percent <br />Impervious <br />14 <br />30 <br />42 <br />80 <br /> <br />Runoff <br />Coefficient <br />0.40 <br />0.45 <br />0.55 <br />0.92 <br /> <br />" <br /> <br />Figure 9: <br />PRECIPITATION. FREOUENCY CURVES for SAND CREEK <br />WATERSHEDS near STERliNG, COLORADO <br /> <br />:5 <br /> <br />16 <br />