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<br />I <br /> <br />I <br /> <br />IV, HYDRAULIC ANALYSIS <br /> <br />Computer runs were made in the upstream direction for flow in the <br /> <br /> <br />sub-critical to critical depth mode, The flow was found to be sub-critical <br /> <br />at the lower end of the study area where backwater is created by the <br /> <br />various culverts. Upstream, the flow tends to oscillate between <br /> <br />sub-critical and critical, <br /> <br />I <br /> <br />I <br /> <br />The flow rates developed in the hydrologic analysis were then used in the <br /> <br />hydraulic analysis to determine the peak water surface profile and flood <br /> <br />plain limits resulting from a 100-year return frequency storm within the <br /> <br />Spring Gulch drainage basin, As mentioned earlier, the existing small <br /> <br />check darns within Spring Gulch have been included in the hydraulic analysis <br /> <br /> <br />since their presence, although probably temporary in nature, could produce <br /> <br />higher water surface profiles and wider flood plain limits until such time <br /> <br /> <br />as the check darns are washed out by flood overtopping, <br /> <br />The HEC-2 computer program utilizes the Manning formula for analyzing the <br /> <br />flood plain hydraulics. A Manning's "n" value of 0.035 was used both for <br /> <br />the main channel and the overbank areas. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Additional studies were performed to determine the maximum water surface <br /> <br /> <br />profile and flood plain limits for backwater conditions which could result <br /> <br /> <br />from the future construction of roadway crossings at various locations <br /> <br /> <br />along the water course. Floodway limits and water surface elevations were <br /> <br /> <br />also evaluated for those areas where future encroachments within the <br /> <br /> <br />overbank portions of the flood plain could cause a rise in the peak water <br /> <br /> <br />surface elevation of up to, but not more than, 0.5 feet above the 100-year <br /> <br />storm water surface elevation without encroachments. <br /> <br />On completion of the HEC-2 computer runs, the water surface profile and <br /> <br />100-year flood plain limits were plott~d on the Flood Hazard Delineation <br /> <br /> <br />drawings provided in the Appendix of this report, Backwater conditions <br /> <br />resulting from tentative culvert-type road crossings have also been <br /> <br /> <br />plotted, The flood plain data used for these plots as well as computed <br /> <br />floodway data are tabulated on the Flood Plain and Floodway Reference Data <br /> <br />sheets, Table 3 which is also included in the Appendix, The culvert type <br /> <br /> <br />road crossing backwater condition referenced above tabulated at the end of <br /> <br />Table 3, Page 3, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Flood plain cross-sections were taken from I inch ~ 40 feet scale <br />topographic maps, These cross-sections were digitized and incorporated <br />into the HEC-2 Water Surface Profiles computer program developed by the <br />Corps of Engineers Hydrologic Engineering Center, Davis, California <br />(Reference E), <br /> <br />V, FLOOD HAZARD AREA DELINEATION <br /> <br />I <br /> <br />A, FLOOD FREOUENCY AND DISCHARGE <br /> <br />I <br /> <br />I <br /> <br />Tentative culvert-type road crossings were evaluated separately assuming <br /> <br />that the individual culverts would be sized such that the resulting <br /> <br /> <br />backwater would peak at an elevation three feet below the minimum roadway <br /> <br /> <br />elevation at the crossing, Spillways might also be provided where <br /> <br /> <br />necessary to assure that the maximum assumed backwater elevation is not <br /> <br />exceeded. The actual sizing of these culverts and spillways is not needed <br /> <br /> <br />for this analysis and will, therefore, be address~d in a later phase of <br /> <br /> <br />development planning, <br /> <br />Floods will continue to occur in the future along Spring Gulch with <br /> <br /> <br />magnitudes equal to and greater than those that have occurred in the past, <br /> <br /> <br />As development progresses within the drainage basin, the flooding potential <br /> <br /> <br />will increase and actual flooding will occur more frequently, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The Spring Gulch drainage basin has been analyzed to determine the <br /> <br /> <br />discharge at various key locations along the Spring Culch channel for the <br /> <br />100-year flood event, The 100-year flood event is defined as that which <br /> <br /> <br />has a one percent chance of being equalled or exceeded in anyone year, <br /> <br />The 100-year flood is considered by the Urban Drainage and Flood Control <br /> <br /> <br />District, the Colorado Water Conservation Board, and the Federal Insurance <br /> <br />Administration, as the flood magnitude for which flood plains should be <br /> <br /> <br />designated for regulatory and improvement purposes. <br /> <br />,I <br /> <br />I <br /> <br />6 <br />