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FLOOD10337 (2)
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Last modified
11/23/2009 12:41:32 PM
Creation date
5/9/2007 2:20:02 PM
Metadata
Fields
Template:
Floodplain Documents
County
Arapahoe
Community
Greenwood Village
Stream Name
Upper Goldsmith Gulch
Title
Flood Hazard Area Delineation, Upper Goldsmith Gulch
Date
4/1/2005
Prepared For
Urban Drainage and Flood Control District, Arapahoe County and Greenwood Village
Prepared By
Moser and Associates
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br /> <br />I <br /> <br />2-1 <br /> <br />I <br />I <br /> <br />vere calculated only for the existing land-use condition due to the area's fully-developed state. <br />'" with District policy, existing privately-owned detention basins were not included in the <br />hydrologic models because of the uncertainty associated with their continued existence. <br />owned and maintained detention basins were included in the models. <br /> <br />lists the one-hour rainfall depths <br /> <br />Additionally, <br />used for the analysis. <br /> <br />hour <br /> <br />storm duration. <br /> <br />maps. <br />the 80th percentile (0.5 <br /> <br />in/hr ) <br /> <br />event was also modeled. <br /> <br />depths <br />Table 2-1 <br /> <br />below <br /> <br />Hydrographs <br />In accordancp <br /> <br />However, <br /> <br />publiclY- <br /> <br />from the USDCM <br /> <br />2.2.4 Rainfall <br />The one-hour rainfall <br /> <br />I-Hour Rainfall <br /> <br />depths for the 2-, <br /> <br />5-, 10-, 25-, <br />The CUHP model <br /> <br />50-, <br /> <br />100-, and 500-year storm <br />then distributed <br /> <br />the <br /> <br />rainfall <br /> <br />events <br /> <br />over a 2- <br /> <br />were gathered <br /> <br />I <br /> <br />adjusting the <br />peak flow at <br />discussed in more detail <br /> <br />in Section 2.4. <br /> <br />Drainage Criteria Manual <br />Appendix A. <br /> <br />I <br /> <br />. . <br />ImpervIOUS <br />Belleview Avenue, <br /> <br />the most <br /> <br />downstream <br /> <br />limit <br /> <br />of this study. <br /> <br />models generate similar <br />The comparison process <br /> <br />IS <br /> <br />(USDCM,200l). <br /> <br />The distribution of the C soil type can be seen on Figure A-3 <br /> <br />In <br /> <br />I <br /> <br />values <br /> <br />The new UDSWM model <br /> <br />was compared to the <br />and the detention characteristics. <br /> <br />1989 UDSWM model by running several different scenarios <br />all the <br /> <br />In <br /> <br />cases, <br /> <br />For Type C <br />These values are <br /> <br />soil <br /> <br />in accordance with District criteria as <br /> <br />the <br /> <br />initial infiltration rate <br /> <br />is 3.0 inches per hour (iph) <br />referenced <br /> <br />in the Runoff Chapter of the Urban Storm <br /> <br />and the final <br /> <br />infiltration rate <br /> <br />is 0.5 iph. <br /> <br />The routing for the Study Area was generated using the <br />Water Management Model (UDSWM). Routing of the peak flows UDSWM model requires <br />information on the physical characteristics of the conveyance system as geometry, roughness, and <br />The existing conveyance system information was formatted for input into the UDSWM <br />runoff hydro graphs generated from the runoff was <br />to obtain peak flow <br /> <br />I <br /> <br />system <br /> <br />rate, <br /> <br />stage data, <br /> <br />the COOP analysis, <br />and time-to-peak flow <br /> <br />information <br /> <br />routed through <br />at specific <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />. <br /> <br />. <br /> <br />Surface retention storage values <br /> <br />Soil <br /> <br />infiltration rates <br /> <br />District's January 1, <br />using the <br />such <br /> <br />2001 <br /> <br />version of the Storm <br /> <br />2.2.3 Soils <br />One soil type <br />Area. Generally, <br />hydrological soil <br /> <br />Appendix A. <br /> <br />fully-developed state. <br />levels of existing imperviousness. <br />to 95 percent. <br /> <br />2.2.2 Watershed Imperviousness <br />The watershed imperviousness was determined <br /> <br />variants (loamy soils) <br /> <br />with a <br /> <br />from <br /> <br />5 <br /> <br />percent <br /> <br />was <br /> <br />only for the existing land-use <br />The mapping provided by the District along with site reviews were used to identify <br />Seven different categories of imperviousness were identified and ranged <br />types and locations A-2 in <br /> <br />The <br /> <br />. . <br />ImpervIOusness <br /> <br />found in the Goldsmith Gulch Study <br /> <br />are <br /> <br />condition due <br /> <br />shown <br /> <br />in Figure <br /> <br />to <br /> <br />the area's <br /> <br />I <br /> <br />. <br /> <br />Time of concentration <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Drainage area <br />Length of the subwatershed <br />Subwatershed <br /> <br />District's 2000 version of the Colorado Urban Hydrograph Procedure <br />in the CUHP analysis include: <br /> <br />2.1 <br />The <br /> <br />for each subwatershed <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br /> <br />. <br /> <br />Percent imperviousness <br /> <br />slope <br />Distance to the sub watershed centroid <br /> <br />Information <br />identified by the Soil Conservation Service (1971) <br /> <br />the predominant soil types are Buick, Fondis, and Renohill <br /> <br />classification of Type C. <br /> <br />5 acres to 82 acres <br /> <br />inspections <br /> <br />contour mapping, provided by the District, <br />were performed to verify flow paths and boundaries. <br />with an average drainage area size of <br /> <br />19.5 acres. <br /> <br />to identify <br />sub watersheds range <br /> <br />The <br /> <br />in size from <br /> <br />METHODOLOGY <br />storm runoff hydro graphs for the sub watersheds <br /> <br />within <br /> <br />the <br /> <br />Study <br />(CUHP) <br /> <br />Area were generated using <br />The physical characteristics <br /> <br />the <br /> <br />The 2-foot <br /> <br />2.2.1 Sub watershed Delineation <br /> <br />A total of 50 subwatersheds were delineated <br /> <br />identification <br /> <br />displayed <br />characteristics of each sub watershed are described <br /> <br />and <br /> <br />locations <br /> <br />are <br /> <br />was used <br /> <br />on Figure A-I <br />in Table A-I <br /> <br />in the Goldsmith Gulch Study <br /> <br />In <br /> <br />Appendix <br />located <br /> <br />subwatershed boundaries. <br /> <br />in Appendix A. <br /> <br />In addition, the physical <br /> <br />sub watershed <br /> <br />A. <br /> <br />Area. <br /> <br />The <br /> <br />Field <br /> <br />I <br />I <br /> <br />SECTION 2 <br /> <br />2.2 <br /> <br />CUHP PARAMETERS <br /> <br />HYDROLOGIC ANALYSIS <br />
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