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FLOOD07906
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Last modified
1/25/2010 7:13:07 PM
Creation date
10/5/2006 3:17:41 AM
Metadata
Fields
Template:
Floodplain Documents
County
Summit
Community
Frisco
Stream Name
Tenmile Creek
Basin
Colorado Mainstem
Title
Flood Hazard Mitigation Tenmile Creek Frisco
Date
5/1/1996
Prepared For
Frisco
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />. <br /> <br />was investigated to see if the levee system along the right bank could be reduced or <br />eliminated. Alternative 3 would be the most expensive alternative. <br /> <br />The three methods were evaluated based on the criteria of rmtlgation benefits, <br />construction methods and costs, and project feasibility. The recommended plan of <br />improvement is presented in section VIII. <br /> <br />VII. ENGINEERING ANALYSES <br /> <br />The lOO-year peak flows used for this study were obtained from the Town of Frisco Flood <br />Insurance Study (FEMA, 1994). A summary of the peak flows is as follows: <br /> <br />Location 100- Year Discharl!e (cfs) <br />Tenrnile Creek at Lake Dillon 1980 <br />Tenmile Creek below North Tenmile Creek 1900 <br /> <br />. <br /> <br />The hydraulic analysis for this study was performed using the U.S. Army Corps of <br />Engineers HEC-2 step-backwater computer program. The base HEC-2 model used for <br />this study was prepared by Muller Engineering Company, Inc. under contract with FEMA <br />for the completion of hydraulic analyses for the Town of Frisco Flood Insurance Study <br />(1994). Three new HEC-2 models (study models) were created by the CWCB for the <br />purposes of this study. The first study model represents revised existing, and the second <br />and third study models represent the proposed conditions which include the alternative <br />mitigation improvements. A floodway analysis was not performed for this feasibility <br />study. The HEC-2 output files for the revised existing conditions and for the proposed <br />conditions (recommended plan only) are included in Appendix A. <br /> <br />Starting water surface elevations for the lOO-year event in the study models were <br />estimated using the slope-area option of HEC-2. Selected "n" values in the revised <br />existing and proposed conditions models were adjusted to improve consistency and to <br />better reflect actual conditions of the channel and overbank areas. A table of "n" values <br />for the effective, revised existing, and proposed conditions HEC-2 models is presented in <br />Appendix B. Three cross-sections were added to the study models based on field <br />surveyed cross-sections obtained by the CWCB. For simplicity, the fill material in the <br />proposed conditions HEC-2 runs were modeled by using X3 cards to block overflow <br />along the right channel bank. <br /> <br />. <br /> <br />The revised existing conditions and proposed models eliminated the right bank split flow <br />that was modeled by Muller Engineering and shown on the effective FIRM panel. The <br />elimination of the split flow can be attributed mainly to the decrease in water surface <br />elevations resulting from the revised "n" values in the CWCB models. The split flow <br />elimination caused a higher discharge and slightly higher water surface elevations in the <br />downstream portion of the stream reach of the main channel from station 0+00 to 13+00. <br />However, there are no anticipated adverse impacts due to the water surface increases in <br /> <br />6 <br />
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