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Last modified
11/23/2009 1:21:20 PM
Creation date
10/4/2006 9:35:30 PM
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Floodplain Documents
County
Larimer
Community
Fort Collins
Title
Precipitaion Frequency Study
Date
7/16/1998
Prepared For
Fort Collins
Prepared By
WRC Engineering, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />2. Two Hour Analyses: <br />Currently, the City of Fort Collins utilizes a two hour design storm for the design of drainage <br />systems in small watersheds. Therefore, a comparison of the resulting 2 hour event data is <br />needed. A direct comparison to NOAA Atlas was not possible in this case since an equivalent <br />period of record, as was used with NOAA Atlas 2. for the period prior to 1948 was not <br />available. Therefore, the analyses were based on the periods ofrecord from 1948 to 1996 and <br />1997. The results are presented in Table 3 and Figures 6 and 7. The supporting analyses are <br />contained in Appendix O. <br /> <br />As with the 24 hour analyses, the Fisher-Tippet distribution tends to replicate the NOAA Atlas <br />2 Fisher-Tippet distribution better, but does not fit the data with the 1997 storm as well as the <br />Log Pearson Type III distribution (Appendix 0). The difference with the 2 hour analysis is <br />that it suggests that NOAA Atlas is overestimating the 2-, 5-, and IO-year return periods, and <br />underestimating the 25-year return period and above for the 2 hour analysis. <br /> <br />B. <br /> <br />CSU ANALYSES: <br /> <br />The analyses contributed by Oli Sveinsson at Colorado State University were done using the same data <br />periods as those used by WRC. Oli's analyses however, focused on the hourly data. "at-site" and <br />regional, using GEV and LN-3 data distributions weighted by L-moments rather than conventional <br />moments. Both of which give a reasonable fit to the data points used. Oli's results are shown in table <br />4 and have been converted from annual series to partial duration where needed. For more information <br />on these analyses, consult appendix F. Oli recommends using a regional GEV analysis of the 2 hour <br />data that includes the 1997 storm as recorded. <br /> <br />Comparing this analysis with WRC's 2 hour Log Pearson III analysis. shows some differences. Figure <br />8 shows that in general. the WRC results match for the 2-year return period, but are significantly <br />higher for the rest of the return periods, with the lOO-year return period being 0.69 inches higher. <br />When WRC's results are compared with Oli's "at-site" analysis, the values are quite similar throughout. <br />Therefore it can be concluded that the differences are attributed mostly with the "at-site" versus <br />regional analysis difference. When discussing the regional analyses. Oli states in his report, "This <br />should indicate that Fort Collins is an extreme compared to the other two stations used in the regional <br />analysis", recommending to stilI use the regional analysis, most likely due to having only 50 years <br /> <br />-7- <br />
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