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<br />2.4 Flood Protection Measures <br /> <br />See Section 10.1. <br /> <br />3.0 ENGINEERING METHODS <br /> <br />For the flooding sources studied in detail in the community, standard <br />hydrologic and hydraulic study methods were used to determine the flood <br />hazard data required for this study. Flood events of a magnitude that are <br />expected to be equaled or exceeded once on the average during any <br />10-, 50-, 100-, or SOa-year period (recurrence interval) have been <br />selected as having special significance for floodplain management and for <br />flood insurance rates. These events, commonly termed the <br />10-, 50-, 100-, and SOO-year floods, have a 10-, 2-, 1-, and O.2-percent <br />chance, respectively, of being equaled or exceeded during any year. <br />Although the recurrence interval represents the long-term average period <br />between floods of a specific magnitude, rare floods could occur at short <br />intervals or even within the same year. The risk of experiencing a rare <br />flood increases when periods greater than 1 year are considered. For <br />example, the risk of having a flood that equals or exceeds the lOO-year <br />flood (1-percent chance of annual exceedence) in any 50-year period is <br />approximately 40 percent (4 in 10); for any gO-year period, the risk <br />increases to approximately 60 percent (6 in 10). The analyses reported <br />herein reflect flooding potentials based on conditions existing in the <br />conununity at the time of completion of this study. Maps and flood <br />elevations will be amended periodically to reflect future changes. <br /> <br />3.1 Hydrologic Analyses <br /> <br />Hydrologic analyses were carried out to establish peak discharge <br />frequency relationships for each flooding source studied in detail <br />affecting the community. <br /> <br />The peak discharges for the 10-, 50-, 100-, and SOa-year floods for <br />Coal Creek used in this study were developed by the SCS in a report <br />entitled "Flood Hazard Analyses, Coal Creek and Rock Creek, Boulder <br />and Weld Counties, Colorado" (Reference 2). The SCS used synthetic <br />rainfall-runoff procedures, as described in the SCS National <br />Enqineering Handbook (Reference 5), and the TR-20 computer program <br />for flood routing (Reference 6) to establish the selected discharges <br />along the stream. <br /> <br />Peak discharge-drainage area relationships for Coal Creek are shown <br />in Table 1. <br /> <br />Analyses were carried out to establish the peak elevation-frequency <br />relationships for each flooding source studied in detail. <br /> <br />3.2 Hydraulic Analyses <br /> <br />Analyses of the hydraulic characteristics of <br />sources studied were carried out to provide <br />estimates of the selected recurrence intervals. <br /> <br />flooding <br />flood <br /> <br />from the <br />elevation <br /> <br />4 <br />