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<br />.--. <br /> <br />however has a difficult time predicting flooding in basins that respond in time scales <br />of less than 2 hours. It is estimated that more than 70 percent of flash flood warnings <br />have less than one-hour lead time; while more than 50 percent of flash flood <br />warnings have no lead time (NWS, ]982). The City of Fort Collins contains thirteen <br />stormwater basins within the City boundary that are considered to be "flashy" in <br />nature (they respond in Jess than I hour). The quick response of these basins is a <br />function ofland development within the basin and the nature of the meteorology of <br />the north-east Colorado front range. <br /> <br />There is a common perception that severe (often flood producing) weather events <br />occur frequently during the first three weeks of June and again in late July and early <br />August along the Colorado and Wyoming Front Range. The Big Thompson flood <br />that killed 139 people occurred on Ju]y 31. ]976. The Fort Collins flood of! 997 that <br />killed 5 people occurred on July 27 and 28. The Fort Collins hail storm that killed <br />one person occurred on July 30, 1979. These severe weather events have been <br />documented (McKee and Doesken, 1997) and are summarized in Table 2 below. <br /> <br />Table 2 <br />Documented Extreme Storm Events <br />(Reproduced from McKee and Doesken, 1997) <br /> <br />Storm Name <br /> <br />Date <br /> <br />Maximum <br />Rainfall <br /> <br />--- <br /> <br />LivermorelBoxelder <br />PueblolPenrose <br />Savageton, WY <br />Cherry Creek/Hale <br />N. Colo. Front Range <br />Rye (S. Ft. Range) <br />Gibson Dam, MT <br />Plum Creek (and others) <br />Big Elk Meadows <br />Rapid City, SD <br />Big Thompson <br />Frijole Creek <br />Fort Collins <br />Pawnee Creek <br /> <br />May 20-21, 1904 <br />June 2-6, 1921 <br />Sep 27-29, ]923 <br />May30-3], ]935 <br />Sept. 2-3, 1938 <br />May 18-20, 1955 <br />June 6-8, 1964 <br />June 16-] 7, ]965 <br />May 4-8, ] 969 <br />June 9, ]972 <br />July 3], ]976 <br />July 2-3, ] 98] <br />July 27-28, ] 997 <br />July 29-30, 1997 <br /> <br />8" (or more) <br />6-12" <br />17" <br />12-24" <br />6-10" <br />6-13" <br />16" <br />14-16" <br />6-14" <br />15" <br />12" <br />8-]6" <br />14.5" <br />15.1" <br /> <br />.--. <br /> <br />Note that the table includes only the largest storm events (most of which had <br />associated fata]ities) and includes all known storms from the Fort Collins region that <br />exceeded] 0 inches of rainfa]1. The table does not include the many storms of the 4-8 <br />inch category that locally may exceed the 100-year storm event. Weaver and <br />Doesken performed an analysis in order to statistically support the hypothesis that <br />severe weather frequently occurs during the first three weeks of June and again in <br />late July and early August (Weaver and Doesken, 1990). The results of their analysis <br />confirmed this hypothesis. A total of 28 out of the 30 years studied experienced <br /> <br />16 <br />