Laserfiche WebLink
FEB-07-1995 09:36 <br />FROM ~ REGION 8 NTFtO TO ~ 913034939213 P. 07 <br />damages Fran the flood were estimated at $602,000. The <br />estimated discharge from this flood was 22,000 cfs at Loveland, <br />larger than the 100-year discharge of 19,000 cfs (Reference 2). <br />The asst recent flood occurred on July 31, 1976, ns torrential <br />rains in the Big Thompson Canyon caused a severe flood, greater <br />than the 100-year flood. A total of 139 people lost their <br />lives. At Loveland, the flood and damage were less severe; <br />however, damages totaled as much as 5500,000 for some businesses <br />(Reference 7). The peak discharge at a gaging station located <br />at the mouth of the canyon was estimated at 31,000 cfs. At <br />Loveland, the peak discharge measured approximately 20,000 cfs, <br />approximately the same as the 1D0-year discharge (Reference 8). <br />2.4 Ftood Protection Measures <br />No flood protection structures exist on the Big Thompson River; <br />however, some protection is provided by weather reports and <br />local watches on stream gages during crucial storm periods <br />(Reference 2). <br />3.b EhGINEER7NG METHODS <br />For the flooding sources studied in detail in the community, standard <br />hydrologic and hydraulic study methods were used to determine the <br />flood hazard data required for this study. Ftood events at a magni- <br />tude which are expected to be equalled or exceeded once on the average <br />during any 10-, 50-, 100-, or 500-year period (recurrence intervals), <br />have been selected as having special significance for flood plain <br />management and for flood insurance premium rates_ These events, <br />commonly teru~ed the 10-, 50-, 100-, and 500-year floods,.have a 10, <br />2, 1, and 0.2 percent chance, respectively, of being equalled or <br />exceeded during arty year. Although the recurrence interval repre- <br />sents the long-term, avers a period between floods of a specific <br />magnitude, rare floods could occur at short intervals or even within <br />the same year. The risk of experiencing a rare flood increases when <br />periods greater than one year are considered. Fo•example. the risk <br />of having a flood which equals or exceeds the 1D0-Year flood (one <br />percent chance of annual occurrence) in any 50-year period is about <br />40 percent (4 in 10), and for arty 90-year period, the risk Increases <br />to about b0 percent (6 in 10). The analyses reported here reflect <br />flooding potentials based on conditions existing in the community at <br />. the time of completion of this study. Maps and flood elevations ::'il <br />be amended periodically to reflect future changes. <br />3.1 Hydrologic Analyses <br />i <br />I-(ydrologiC analyses were carried out to establish the peak <br />discharge-frequency relationships fpr floods of the selected <br />recurrence intervals for each flooding source studied in detail <br />affecting the community, <br /> <br />I <br />i <br />