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FLOOD00385
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Last modified
11/23/2009 1:21:52 PM
Creation date
10/4/2006 9:15:03 PM
Metadata
Fields
Template:
Floodplain Documents
County
Boulder
Community
Boulder
Stream Name
Boulder Creek
Title
South Boulder Creek Interim Hydrology Study
Date
7/1/2000
Prepared For
Boulder County
Prepared By
Taggart Engineering Associates, Inc.
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />1- 14 <br /> <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 />DISCHARGE PROFILES <br /> <br />The discharge profiles for South Boulder Creek and the West Valley Overflow are <br />presented in Figures 1-1 and 1-2, respectively. Stationing along South Boulder Creek <br />begins at the confluence with Boulder Creek and increases going upstream. The <br />significant spill from South Boulder Creek to the West Valley Overflow begins <br />approximately at Station 359 + 50 on South Boulder Creek. <br /> <br />The Figure 1-1 South Boulder Creek discharge profile shows four major spills to the <br />West Valley Overflow: two upstream of Highway 93, one upstream of Highway 36, <br />and one downstream of the Wellman to the golf course. Two major inflows occur: <br />one from the West Valley Overflow in the area of the middle levee on CU's <br />property, about 1500 to 2000 feet upstream of Highway 36, and the <br />Viele/Anderson Ditch inflow which carries some of the West Valley Overflow <br />discharge back to South Boulder Creek. There are also several tributary basin <br />inflows, such as David's Draw and the areas along South Boulder Creek. <br /> <br />The Figure 1-2 discharge profiles show the spills from South Boulder Creek above <br />Highway 93 and Highway 36, and the flows returning to South Boulder Creek nes.r <br />the CU middle levee and the Viele channel and Anderson Ditch. At Baseline the <br />West Valley Overflow spills seven different ways, three of which can send portions <br />of their discharges to Bear Canyon Creek. Some of this flow, and flood discharges <br />following other routes, discharge to the Wellman Ditch, with a portion of the total <br />flow going north to Boulder Creek through neighborhoods midway between 55th <br />and Foothills. From Foothills and Baseline, the West Valley Overflow discharge <br />only reflects the estimated portion of the West Valley Overflow following the <br />Crossover Ditch and Dry Creek Ditch No.2. The discharge drops to nil (30 cfs) for <br />the flow crossing under the Wellman. Thus, of all the flow arriving in the West <br />Valley Overflow to Foothills and Baseline, most spills to Bear Canyon Creek or the <br />Wellman Ditch, with portions of the Wellman overflow going north to Boulder <br />Creek. Downstream of the Wellman the route along Dry Creek Ditch No.2 <br />increases as the Wellman spills just upstream and downstream of 55th, and <br />increases again midway across the golf course due to the South Boulder Creek spill. <br /> <br />MODEL REASONABLENESS AND REFINEMENT <br /> <br />Detailed model verification and reasonableness evaluations are presented in <br />Section V for individual basins, comparative Colorado Unit Hydrograph Procedure <br />(CUHPj modeling for representative tributaries, for regional relations developed by <br />CWCB, and other unit discharge (ets/acre) comparison. It appears the results are <br />reasonable for the tributary watersheds. <br />
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