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FLOOD10363 (2)
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Last modified
11/23/2009 12:49:17 PM
Creation date
7/13/2007 9:28:00 AM
Metadata
Fields
Template:
Floodplain Documents
County
Gunnison
Community
Gunnison County
Stream Name
East River, Cement Creek, Alkali Creek, Ohio Creek
Title
Gunnison County Flood Hydrology, Contract # W99-D-0018 Final Report
Date
11/1/2004
Prepared For
US Army Corps of Engineers, CWCB and Gunnison County
Prepared By
Tetra Tech, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br /> <br />I <br />I <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />EXECUTIVE SUMMARY <br /> <br />Gunnison County is currently preparing floodplain information for use in updating the Federal Emergency <br />Management Agency (FEMA) Effective Flood Insurance Study (FIS) and associated maps. In doing so, <br />Gunnison County identified eight river reaches for inclusion in the updated FIS. This report presents an <br />unimpaired and natural flow analyses for the natural flow of the eight stream reaches in Gunnison County. <br />Flood frequency analyses are completed for the 10, 2, 1, and 0.2 percent chance exceedence events for <br />each reach. The study is part of the U.S. Army Corps of Engineers', Floodplain Management Services <br />Program, and is being conducted for the City of Gunnison, Gunnison County, and the Colorado Water <br />Conservation Board. <br /> <br />The Gunnison River and Tomichi Creek within the boundaries of the City of Gunnison have been included <br />in two previous hydrologic studies. The first study was conducted by Engineering Consultants, Inc. in <br />1977 for the City of Gunnison, Gunnison County, and the Colorado Water Conservation Board. The <br />second study was conducted by FEMA in 1982. These two reaches are the only reaches included in this <br />current study that have been analyzed in the past. Since the time of those studies, the area has <br />experienced some above average annual peak flow values that affect the hydrologic analysis and <br />resulting floodplain inundation, thus warranting a revised study. <br /> <br />Two of the eight stream reaches are analyzed using available peak flow information from streamgage <br />records. The other six reaches have insufficient streamgage data and are therefore analyzed using <br />expanded data series and correlations with available streamflow data from adjacent reaches. Procedures <br />are presented in Section 4.0. Results are presented in detail and summarized in Section 5.0, and noted <br />in Table ES.1. <br /> <br />The study also includes a review of the recorded streamflow data to determine the attenuation effects on <br />the flow data caused by the Taylor Park Dam located on the Taylor River. This is a Bureau of <br />Reclamation irrigation storage reservoir for the Uncompahgre Valley Project. Construction of the dam and <br />reservoir began in 1935 and the first releases were made in 1937. The primary purpose of Taylor Park <br />Dam is irrigation supply. The operating schedule is not designed for flood control; however, the storage <br />capacity of the reservoir does impact flood flows in downstream study reaches along the Taylor and <br />Gunnison Rivers. Thus, stream flow records are adjusted to remove the influence of the reservoir on flood <br />peaks using a combination of flow records and reservoir storage records. <br /> <br />A review of the nature of flood events is also completed in regards to snowmelt and rain on snow event <br />flows. The review shows that the hydrology of the streams in this system is driven by snowmelt runoff, the <br />peak of which typically occurs between March and June (with a few peaks occurring in early July). Rain <br />on snow, defined as 0.5 inches of rainfall or greater for this study, occurs infrequently. For example, the <br />Tomichi Creek, with a large percent of watershed in high mountain valley, had eight out of sixty-three <br />years of peak values caused by rain on snow event flows. Two analyses are performed: one with data <br />sets including the rain on snow peaks, a second using only snowmelt peaks. The results, while similar, <br />indicate that rain on snow event flows have a discernible effect on the resulting flood frequency statistics <br />for the reach. Therefore, the 0.5-inch precipitation threshold was used to filter the data for the remaining <br />reaches for rainfall on snow events. <br /> <br />This study provides the necessary flood flows to complete the analyses of the hydraulics for the FEMA <br />FIS study along each of the eight reaches for the associated flood events. <br /> <br />v <br />
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