Laserfiche WebLink
<br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of flooding <br />sources studied were carried out to provide estimates <br />elevations of floods of the selected recurrence intervals. <br /> <br />from <br />of <br /> <br />the <br />the <br /> <br />For the original study, water-surface elevations were computed for <br />the 10-, 50-, 100-, and 500-year floods using the COE HEC-2 <br />computer program (Reference 11). <br /> <br />For Coal Creek, a culvert at the southern <br />County Road 62, was used as a control, <br />elevation at its inlet was used as the <br />elevation. <br /> <br />corporate <br />and the <br />starting <br /> <br />1 imi t s, under <br />water-surface <br />water-surface <br /> <br />Cross section data for streams in the area were obtained from <br />topographic maps at a scale of 1:2,400, with a contour interval of <br />2 feet (Reference 12). All bridges and culverts were surveyed to <br />obtain elevation data and structural geometry. <br /> <br />The COE HEC-2 computer program was also used to perform water- <br />surface profile computations for the restudy of Boxelder Creek. <br />Numerous bridges and culverts exist along the channel through the <br />study reach. Those that created significant backwater effect were <br />handled in the HEC-2 analysis with appropriate bridge routines. A <br />few bridges and culverts are only minor segments of the total <br />floodplain, and, therefore, were considered in the Mannings <br />retardance factor rather than in separate bridge analyses. <br /> <br />Cross section data and reach length information were obtained from <br />photogrammetric maps prepared especially for the SCS study <br />(Reference 1). Hydraulic roughness coefficients ("n" values) were <br />determined from field inspection. <br /> <br />Locations of selected cross sections used in the hydraulic analyses <br />are shown on the Flood Profiles (Exhibit 1) and on the FLood <br />Insurance Rate Map. <br /> <br />The hydraulic analyses for this study were based on unobstructed <br />flow. The flood elevations shown on the profiles are thus <br />considered valid only if hydraulic structures remain unobstructed, <br />operate properly, and do not fail. <br /> <br />All elevations are referenced to the National Geodetic Vertical <br />Datum of 1929 (NGVD). Elevation reference marks and the <br />descriptions of the marks used in this study are shown on the maps. <br /> <br />4.0 FLOODPLAIN MANAGEMENT APPLICATIONS <br /> <br />The NFIP encourages State and local governments to adopt sound <br />floodplain management programs. Therefore, each Flood Insurance Study <br />provides lOO-year flood elevations and delineations of the 100- and 500- <br />year floodplain boundaries and 100-year floodway to assist communities <br />in developing floodplain management measures. <br /> <br />7 <br />