Laserfiche WebLink
<br />WATTENBERG, COLORADO FLOOD HAZARD MlTIGA TlON PLAN <br /> <br />AUGUST 1996 <br /> <br />as the floodplain concept provides a national <br />standard for the National Flood Insurance <br />Program (NFIP). <br /> <br />FLOOD RECURRENCE INTERVALS <br /> <br />10- Year Flood Recurrence interval of <br />about 10 years but a"} 0% <br />chance of occurring in any <br />year. <br /> <br />50- Year Flood Recurrence interval of <br />about 50 years but a 2 % <br />chance of occurring in any <br />year. <br /> <br />1 00- Year Flood Recurrence interVal of <br />about 100 years but al % <br />chance of occurring in any <br />year. <br /> <br />500- Year Flood Recurrence interval of <br />about 500 years but a .2% <br />chance of occurring in any <br />year. <br /> <br />Figure 5 <br /> <br />The 100-year floodplain located within the <br />Community of Wattenberg has been mapped <br />and is printed in the 1979 Flood Insurance <br />Study conducted by the Federal Emergency <br />Management Agency (FEMA) (See Figure <br />6). It is critical, however, for the floodplain <br />residents to remember that floods greater <br />than the standard 100-year flood event may <br />occur at any time. <br /> <br />Types of Floods <br /> <br />Floods occur on nvenne systems. <br />Commonly, a nver basin is fed by a <br />hierarchical order of stream channels that <br />convey the normal flow of water from <br /> <br />smaller watersheds contained within the <br />basins. Flooding results when the flow of <br />water becomes greater than the carrying <br />capacity of the individual stream channel. <br />Rate of rise, peak discharge (magnitude), <br />duration, and frequency of floods, are all a <br />function of physical features and weather <br />conditions which contribute to the volume of <br />water in the river system. The following <br />describes sources of riverine floods which <br />can effect Wattenberg: <br /> <br />Snow-Melt Floods - Snow-melt flooding <br />typically occurs May through June. <br />Generally, this occurs when warm spring <br />temperatures create a fast snow-melt and/or <br />a combination of spring runoff and rainfall <br />over the affected watershed. Serious <br />flooding can result when heavy spring rain <br />accompanies a snow-melt in May and June. <br /> <br />Flash Floods - These floods result from <br />intense summer thunderstorms. This flood <br />event is characterized by an intense <br />cloudburst, a sudden rise in stream level, <br />short duration, and almost no warning. <br />Typically, the flash flood season in Colorado <br />stretches from May through September. <br /> <br />General Rain Floods - These floods are <br />caused by general rainfall events that occur <br />over a wide geographic area for several days, <br />completely saturating the shallow soils. <br />These floods are characterized by a slow, <br />steady rise in the stream level and a peak <br />discharge of long duration. The slow rise <br />rate of the stream provides time for warning. <br /> <br />Flood History of Wattenberg and <br />Weld County <br /> <br />As discussed previously, flooding presents a <br />potential problem in Wattenberg and <br /> <br />6 <br />