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<br /> c c c " " <br />c ~ ~ ~ ~ L <br />~ ~ ~ " " <br />" ~ i .. .. ~ <br />i .. .. <br />0: 0: 0: 0: <br />) ~ ~ L L L <br />" " a a <br />~ .. ~ ~ <br />>- <br />0 ~ ~ '" Q '" 0 <br />0 '" <br />'" 0 <br /> 0 <br /> CD <br />IA!JQ IU!^ <br /> ~ <br /> <br />I. <br /> <br />I <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br />. <br /> <br />I <br /> <br />1111 'oS '9'00 <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />. <br /> <br />1>1 ~OM~&'H <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br /> <br />~ <br />'" <br /> <br />@ <br />'" <br /> <br />8 <br />., <br /> <br />o <br />o <br /> <br />~ <br /> <br />8 <br />'" <br /> <br />(IJO) 3e~YHOSIO <br /> <br />~B <br /> <br />8 <br />o <br />ID <br /> <br /> I <br /> . <br /> . <br /> . <br /> . <br /> g . <br />~ i <br />- I <br />.. <br />.. <br />- <br />- <br />~ Q <br />2 ~ I <br />::::i <br />~ 9 <br />0 I&l <br />::l ~ <br />lii '. <br />::IE ~ <br />c( ~ <br />l&.J <br />a:: . <br />lii <br />z <br />~ <br />0 II: I <br />0 I&l <br />l&.J Q. <br />f) 8 <br />m I <br />c( u) <br />l&.J I&l <br />(,) -' <br />z <br />i! iL '. <br />Ul f <br />0 <br /> I&l I <br /> ~ <br /> c <br /> 0 I <br /> C/) <br /> 0 <br /> ...: I <br /> I&l <br /> II: <br /> 5 . <br /> iL <br /> I <br /> . <br /> <br />29 <br /> <br />Creek, Figure 9 for Cooper Slough with existing basin conditions, and Figure <br /> <br />10 for Cooper Slough with developed basin conditions. <br /> <br /> <br />A detailed description of the methodology used and parameter values is <br /> <br /> <br />given in the "Technical Addendum." <br /> <br />8 <br />~ <br /> <br />Hydraulic Analysis <br /> <br />The analysis of the hydraulic characteristics of Boxelder Creek and <br /> <br /> <br />Cooper Slough were conducted to determine the water surface elevation for peak <br /> <br /> <br />flows of the 2-, 10-, 25-, 50-, 100-, and 500-year floods. The water surface <br /> <br /> <br />elevations were computed using the U.S. Army Corps of Engineers' HEC-2 water <br /> <br /> <br />surface profile computer program (reference 17). Cross sections of Boxelder <br /> <br /> <br />Creek and Cooper Slough were taken from topographic maps (1" = 1 00', 2-foot <br /> <br /> <br />contours) provided by Larimer County, except for a one-half mile reach above <br /> <br />Vine Drive on Cooper Slough where the cross sections were obtained from a <br /> <br /> <br />field survey. Additional cross sections from a field survey were used in con- <br /> <br /> <br />junction with topographic mapping for the area south of State Highway 14 on <br /> <br /> <br />Cooper Slough. Bridge and culvert geometries were field measured. Elevations <br /> <br />for top of the road crossings and downstream and upstream channel inverts were <br /> <br /> <br />surveyed. Roughness coefficients were selected after field investigation and <br /> <br /> <br />analysis of photographs taken during field reconnaissance. The roughness <br /> <br /> <br />coefficients used have been presented in a separate report entitled "Docu- <br /> <br />mentation for Selection of Manning's Roughness Coefficients for Boxelder Creek <br /> <br /> <br />and Cooper Slough" (reference 16). The range of roughness values is given in <br /> <br />Tahle 9. <br /> <br />8 <br />.. <br /> <br />o <br />o <br />o <br />., <br /> <br />o <br />o <br />o <br />'" <br /> <br />At several locations along Boxelder Creek and Cooper Slough, some flow <br /> <br /> <br />leaves the channel because of the limited capacity of bridges or culverts. A <br /> <br /> <br />separate analysis was conducted to determine the flow split at these loca- <br /> <br /> <br />tions. Major flow splits on Boxelder Creek occur at 1-25 and Prospect Street. <br /> <br /> <br />Table 10 lists the flow split data for Boxelder Creek. The flow was not <br /> <br /> <br />traced since the water does not,return to the Boxelder Creek floodplain. <br /> <br /> <br />Splits occur on Cooper Slough at the Colorado and Southern Railroad and at <br /> <br /> <br />State Highway 14. The flood water that overtops Highway 14 flows along three <br /> <br /> <br />separate channels. Separate hydraulic analyses were performed to determine <br /> <br />the water-surface elevations along each individual char-nel. Table 11 lists <br /> <br /> <br />the location and quantity of these flow splits for Cooper Slough. These flows <br /> <br />were traced because the water returns to the Cooper Slough floodplain. <br /> <br />o <br />~ <br />