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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />17th Street to the downstream Arapahoe Road bridge. <br /> <br />A 100-year discharge of 12,000 c.f.s. was used for all reaches <br /> <br />under investigation. <br /> <br />While endorsing the concept of Plan II upstream from l7th Street, <br />the City is concerned that the degree of environmental disturbance <br /> <br />be minimized. A particular item of concern is the loss of trees <br /> <br />l. Flood Plain and Floodway Data <br />The limits of flooding anticipated during the lOO-year dis- <br />charge of l2,000 c.f.s., as determined by the Corps of Engineers, <br /> <br /> <br />are outlined on the attached drawings and tabulated in Table <br /> <br /> <br />1 in Appendix C, Flood Plain and Floodway Reference Data. The <br /> <br /> <br />table lists potential 100-year flood elevations, flooding <br /> <br /> <br />widths and reference line (thalweg) elevation for each cross- <br /> <br /> <br />section within the Study area. The flood profile thalweg <br /> <br /> <br />(reference) line and flood plain width at any point within the <br /> <br /> <br />Study area is graphically presented in the drawings. <br /> <br />and other vegetation. <br /> <br />C. GENERAL APPROACH <br />The existing 100-year flood plain and floodway were previously <br />analyzed by the United States Corps of Engineers using the HEC-2 <br />Water Surface Profile Computer Program and were not re-investigated <br />for this Study. The HEC-2 program was developed by the Corps of <br />Engineers at the Hydrologic Engineering Center in Davis, California, <br />and has been accepted as one of the methodologies for calculating <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />water surface profiles in natural channels. <br />'. <br /> <br />The Corps of Engineers have also determined the floodway for <br /> <br /> <br />Boulder Creek under existing conditions. A floodway represents <br /> <br /> <br />that part of the flood plain which is required to pass a 100- <br /> <br /> <br />year flood event without rasing the flood profile more than <br /> <br /> <br />acceptable amount and which represent hazards to personal <br /> <br />safety and welfare. In this Study, the floodway represents <br /> <br />that portion of the flood plain where the lOO-year flood <br />velocities exceed two feet per second, where the depth exceeds <br /> <br />two feet or where the water surface would not increase more <br /> <br />than one-half feet after encroachment. Floodway widths, <br /> <br />representing the limits of encroachment into the flood plain <br />are tabulated in Table 1 of Appendix C. Water surface elevations <br /> <br />anticipated after encroachment are also tabulated. <br /> <br />The residual flood plain, the flood plain remaining after proposed <br /> <br /> <br />master plan improvements have been implemented, was evaluated <br /> <br /> <br />during the course of this study using the HEC-2 Water Surface <br />Profi le Computer Program. Input to the HEC-2 program included <br />discharge, cross-sectional data, data associated with drainage <br /> <br />structures, obstructions such as buildings, vegetation and manmade <br /> <br />embankments, and channel roughness coefficients. The Manning's <br /> <br />roughness coefficients used in the water surface profile computa- <br /> <br />tions varied from 0.037 to 0.055 in the vicinity of the main channel <br />0.045 to 0.078 for the overbank areas. Transition coefficients <br />used to account for the effects of changing channel geometry on the <br /> <br />energy losses associated with flow were 0.3 for expansion and O. 1 <br /> <br />for contraction. <br /> <br />33 <br />