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Last modified
1/25/2010 7:10:15 PM
Creation date
10/5/2006 2:34:55 AM
Metadata
Fields
Template:
Floodplain Documents
County
Larimer
Community
Wellington
Stream Name
Boxelder Creek
Basin
South Platte
Title
Boxelder Creek Watershed Hydrologic Analyses
Date
12/1/1998
Prepared For
FEMA
Prepared By
UDFCD
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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />DRAINAGE CRITERIA MANUAL <br /> <br />Attachment 4 <br /> <br />RUNOFF <br /> <br /> <br />is <br /> <br />4.14 Basis for 1982 Version of CUHP <br />Rainfall and runoff data were collected by U.S. Geolo9ical survey in the <br />Denver metropo 1 i tan area since 1969 under a cooperat i ve a9reement wi th the <br />Urban Drainage and Flood Control District. Analysis of this data by the <br />District staff began in earnest in 1977. Of the original thirty gaging <br />stations, data from only seven sites (nine different basin conditions) were <br />used by the District to develop the 1982 version of the CUHP. Data from all <br />other sites were evaluated and were determined not suitable for use due to <br />various gaging problems and watershed definition problems. Because the <br />metropolitan area data base lacked an undeveloped watershed, data from a small <br />watershed (Kiowa Creek Tributary at Elbert) being gaged by USGS for the <br />Colorado Highway Department was used to round out the mix of land uses in the <br />data base. <br />Table 4-7 presents a summary of rainfall/runoff data base and includes <br />the key watershed parameters for each site. For each of the dates that data <br />were available, a complete rainfall depth record and concurrent flow <br />measurements at 5-minute time increments served as the basis for the <br />development of the revised CUHP. Peak flows from each recorded hydrograph are <br />compared with the calculated peak flows using the 1982 version of CUHP in <br />Figure 4-8. This comparison substantiates the validity of the new CUHP <br />procedure. <br />Those wishing to compare the older version of the CUHP with the new <br />version will find that often the new unit hydrograph will have a significantly <br />shorter time to peak. This is particularly true for smaller urbanized basins. <br />However. the new vers i on will often produce peak flow results comparable to <br />those obtained using the old version over a wide range of watershed conditions <br />typically used in drainage studies in the Denver Metropolitan Area. <br /> <br /> <br />5-1-84 <br />
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