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Last modified
1/25/2010 6:48:39 PM
Creation date
10/5/2006 1:22:03 AM
Metadata
Fields
Template:
Floodplain Documents
Designation Number
86
County
Arapahoe
Community
Littleton
Stream Name
Lee Gulch and Little Creek
Basin
South Platte
Title
Flood Hazard Area Delineation - Lee Gulch and Little Creek, Littleton, Arapahoe County, CO
Date
10/1/1977
Designation Date
11/1/1977
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 />railroad crossings along Little Creek. A storm drain between <br />Dry Creek Road and the Highline Canal discharges directly in- <br />to the canal and the channel at Sterne Park discharges direct- <br />ly into the City Ditch. The drainage structures along Little <br />Creek are generally inadequate to pass even the high fre- <br />quency storm flows with the exception of the AT&SF Railroad <br />crossing. <br />D. FLOOD HISTORY <br />Little information is available about past flooding on Lee <br />Gulch or Little Creek, particularly floods from low frequency <br />storms. The trans-basin diversion of storm flows by the <br />Highline Canal and the City Ditch, especially in the Little <br />Creek Basin, has probably dampened the flooding effects of <br />both streams, though this has undoubtedly contributed to <br />flooding downstream of both canals. Nuisance flooding has <br />occurred from minor storms in downtown Littleton and on Lee <br />Gulch near Gallup Street. <br /> <br /> TABLE I <br /> HYDROGRAPH PARAMETERS <br /> Length to <br />Sub- Area Length Centroid Slope % Ct Cp <br />Basin (Sq.Mi. ) (~1i. ) (Mi. ) (%) Imp. <br />LEE GULCH <br />1000 0.40 1.52 0.76 1.2 31 0.54 0.66 <br />2000 0.63 1. 33 0.66 2.6 36 0.45 0.62 <br />3010 0.72 1. 61 0.83 2.6 47 0.37 0.56 <br />3020 0.27 1.21 0.59 3.1 67 0.27 0.49 <br />3030 0.40 0.99 0.33 0.1 74 0.53 0.66 <br />4000 0.20 0.59 0.21 3.9 41 0.39 0.58 <br />LITTLE CREEK <br />100 0.12 0.64 0.26 1.0 95 0.23 0.46 <br />200 0.62 1.48 0.78 1.2 39 0.45 0.62 <br />300 0.83 1. 33 0.52 1.6 45 0.40 0.59 <br />410 0.57 1.28 0.52 1.9 42 0.43 0.61 <br />420 0.30 0.97 0.47 2.1 52 0.36 0.56 <br />500 0.29 0.80 0.28 2.7 41 0.41 0.59 <br />NOTE: Parameters are based upon future land use. <br /> <br />III. HYDROLOGY <br /> <br />Rainfall data was obtained from the Rainfall-Depth-Duration- <br />Frequency Maps in the "Urban Storm Drainage Criteria Manual". De- <br />viations between the upper and lower portions of basins were be- <br />tween 0 and 0.2 inches and did not warrant using separate rainfall <br />intensities over the basin. Consequently, the upper basin, or <br />slightly higher values, were used. A three hour duration storm <br />was used. The rainfall data is summarized below: <br />Rainfall Duration <br />6 Hour <br /> <br />Return Frequency <br /> <br />2 Year <br />10 Year <br />100 Year <br /> <br />1 Hour <br /> <br />24 HOLlr <br /> <br />A hydrological analysis of both basins was completed to de- <br />termine the peak discharge-frequency relationship for floods of <br />the 2, 5, 10, and 100-year recurrence intervals. These peak dis- <br />charges were predicated upon full development of the basins with <br />future land use determined from the City of Littleton and Arapahoe <br />County master plans. <br />The Cblorado Urban Hydrograph Procedure as described in the <br />"Urban Storm Drainage Criteria Manual" (revised 5/15/75) and in- <br />terim guidelines furnished by the UDFCD were used to obtain storm <br />hydrographs for each sub-basin. Basin and sub-basin boundaries <br />are shown on Sheet 1 of the drawings and hydrograph parameters <br />are shown in Table I. <br /> <br />1.0 <br />2.1 <br />2.7 <br /> <br />1.6 <br />3.3 <br />4.3 <br /> <br />2.1 <br />3.7 <br />4.7 <br /> <br />The storm hydrographs of the sub-basins were routed and com- <br />bined using the Convex Method of Stream Routing of the Soil Con- <br />servation Service and the Modified PuIs Method of Reservoir Rout- <br />ing to obtain peak discharges at the various hydrological points. <br />Typical flood hydrographs are shown on Figures I.A. and I.B., and <br />peak flow profiles on Figures II.A. and II.B. It was assumed <br />that all trans-basin conveyance of storm runoff by agricultural <br /> <br />-4- <br />
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