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<br />Federal Emergency Management Agency - Letter of Map Revision <br />Two-Mile Canyon Creek - Boulder, Colorado <br />Page 3 <br /> <br />3.0 ENGINEERING METHODS <br /> <br />3.1 HydrolOlnc Analysis <br /> <br />The hydrologic analysis for this study wall taken from the existing Flood Insurance <br />Study (FIS) for the City of Boulder, Boulder Colorado, Community Number 080024 <br />dated May 3, 1990 (Reference 2). <br /> <br />Peak discharge-drainage area relationships for this n:ach are shown in Table 1. <br /> <br />3.2 Hydraulic Analysis <br /> <br />Water surface elevations of the selected recurrence interv;als were computed using the <br />USACE HEC-2 step-backwater computer program (Reference 3). Cross sections <br />used in the backwater analyses for the study were developed using aerial photography <br />compiled in October 1981 (Reference 4) and supple:mented with on-site field <br />surveying at selected locations. <br /> <br />Cross sections from the original flood insw:ance sUldy were used, where applicable. <br />In most cases, the original cross sections were rotated to reflect the actual field <br />conditions based on the aerial topography. Additional cross sections were added at <br />the roadways where needed to depict roadway overtopping conditions. <br /> <br />A split flow analysis has been utilized between 13th Street and 8th Street. <br />Overtopping of the right overbank is present at the 90 degree bend in the channel. <br />The HEC-2 analysis indicated that approximately 25% of the 100-year flow escapes <br />the main channel at this location and continues along 8th Street and Hawthorne <br />Avenue until rejoining the main channel flows at 13th Street (please see "Hawthorne <br />Street Multiple Profile Run, Appendix). <br /> <br />Location of selected cross sections used in the hydraulic analyses are shown on the <br />Flood Boundary and Floodway Maps (Exhibit 1). <br /> <br />Roughness factors (Manning's "n") used in the hydraulic computations wl~re taken <br />from the existing study and confirmed by :field observation. Roughness values for <br />this study range from 0.02 to 0.10. <br /> <br />Starting water surface elevations develop(:d for the previous study were utilized in <br />this re-analysis. <br /> <br />The hydraulic analyses for this study is based on fully obstructed culverts, as <br />determined by the City of Boulder through field inspections. <br /> <br />All elevations are referenced to the National Geodetic Vertical Datum of 1929 <br />(NGVD). Elevation reference marks used for this study are shown on the Flood <br />Boundary and Floodway Maps (Exhibit 1). <br />