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<br />developed hydrologic models for the 10-, 50- and lOa-year storm events. As a part of t <br />project, the SOO-year storm was estimated using flood frequency analysis based on the 10- <br />50- and lOa-year storm events. <br /> <br />HYDROLOGIC ANALYSIS <br /> <br />3. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The Original Report identified a 400-cfs spill flow from Fourmile Canyon Creek to <br />Wonderland Creek at Broadway and additional spill flows at 19th and 26th Streets. However, <br />the Original Report did not reduce the flows in Fourmile Canyon Creek to account for these <br />spill flows. <br /> <br />Model <br /> <br /> <br />Corrected H <br /> <br />3.3.2 <br /> <br />GENERAL <br /> <br />The hydrologic model previously prepared for Fourmile Canyon Creek, as documented in the Major <br />Drainageway Planning. Boulder and Adjacent County Drainageways. Phase B report, dated May of <br />1987, (hereafter referred to as the Original Report) was utilized as the hydrological basis of this <br />study. The input parameters of the Original Report were checked for reasonableness and corrections <br />were made, where appropriate. The Original Report assumed, incorrectly, that all floodwaters <br />remained in the Fourmile Canyon Creek floodplain. The hydrology model for this study was <br />modified as a part if this project to account for flows that spill from Fourmile Canyon Creek and flow <br />into the Wonderland Creek drainage <br /> <br />3.1 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The original hydrologic model was re-created by entering the input parameters from the <br />Original Report into the latest versions of the CUHP hydrologic catchment modeling and the <br />UDSWM hydrologic routing models. "Corrected" CUHPF9S and UDSWM9S computer <br />models were re-created for the 2-, 5-, 10-, 50- and lOa-year storm events <br /> <br />The CUHP input parameters were checked for reasonableness and corrections were made, <br />where appropriate. Based on an analysis of aerial photography, dated October 1998, it was <br />determined that imperviousness of 12% for Sub-catchment 905 was too low. The models <br />were updated with a weighted imperviousness of33% <br /> <br />The hydrologic analysis was completed for the entire Fourmile Canyon Creek watershed. The <br />watershed boundaries are shown in Figures 3-1a and 3-1b. The total tributary area of the Fourmile <br />Canyon Creek watershed is approximately 10.2 square miles. The area tributary to the study reach is <br />approximately 9.24 square miles. Fourmile Canyon Creek discharges to Boulder Creek below State <br />Highway 119. <br /> <br />I <br /> <br />I <br /> <br />The UDSWM input parameters were checked for reasonableness and corrections were made, <br />where appropriate. Based on the City of Boulder's current base mapping, flown May 1993, it <br />was determined the slope of 17% for the conveyance element between Sub-catchments 903 <br />and 904, was in error. The models were corrected with a slope of 1.7%. Channel roughness <br />coefficients were changed from 0.045 to 0.056 and overbank roughness coefficients were <br />changed from 0.06 to 0.075 to approximate the routing of the original HEC-l model. <br /> <br />" <br /> <br />Fourmile Canyon Creek is unique in that a portion of the existing channel is perched within an <br />alluvial floodplain. The perched portion of the channel occurs from the mouth of the canyon <br />downstream to approximately 19th Street. In this reach, once the channel capacity is exceeded, flood <br />flows overtop the south bank and flow in a southeasterly direction towards Wonderland Creek. The <br />result of these spills is flows in Fourmile Canyon Creek downstream of the spill locations are <br />reduced, while the flows in Wonderland Creek are significantly increased. <br /> <br />Analysis <br /> <br />Supporting figures and documentation are presented in Appendix A, ''Hydrologic <br /> <br />SPILL FLOWS <br /> <br />3.2 <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />ic Predictions <br /> <br />Existing development within the study area is predominately residential development with <br />some commercial development near Broadway. The study area is predominately built-out. <br />Development is unlikely to occur within large parcels of open space that have been designated <br />near the mouth of the canyon and in the vicinity of 47th Street and State Highway 119. With <br />the exception of minor in-fill and redevelopment, future land use will remain very similar to <br />existing land use patterns <br /> <br /> <br />Future Land Use H <br /> <br />3.3.3 <br /> <br />With one exception, the spills do not return to Fourmile Canyon Creek. The one exception occurs in <br />the vicinity of the Crestview Elementary School. Spills, which leave Fourmile Canyon Creek <br />between Broadway and 19th Street, flow in a southeasterly direction towards the school. The school <br />acts as a barrier and a further split in the floodwaters causes a portion of the spills to flow north <br />around the school and re-enter Fourmile Canyon Creek. The remaining portion of the spills move <br />southward around the school towards Wonderland Creek. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Imperviousness for future development conditions was estimated by analysis of the City of <br />Boulder North Boulder Sub-Community Plan and Boulder County future zoning maps. The <br />estimated future imperviousness values were input into the CUHPF9S model to determine the <br />peak flows under future land use conditions <br /> <br />HYDROLOGIC ANALYSIS <br /> <br />Model <br /> <br />ic <br /> <br /> <br />Ori <br /> <br />3.3.1 <br /> <br />3.3 <br /> <br />I <br /> <br />the corrected <br /> <br />Report and <br /> <br />the Original <br /> <br />Table 3-1 summarizes the lOa-year flood peaks from <br />and future land use hydrologic models. <br /> <br />Love & Associates, Inc. obtained the technical notebook containing the hydrologic models <br />prepared by MSM/Greiner in 1983 for the Original Report. The Original Report's hydrology <br />was modeled using CUHP-B and routing was modeled using HEC-1 The original report <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />3-1 <br /> <br />I <br />