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<br />I <br /> <br />I <br />. <br /> <br />I <br /> <br />4/8/05 <br /> <br />This FHAD includes prediction of 0.2 percent annual probability (500-year recurrence) flows for the South Platte <br />River that were not included in the Master Plan hydrologic modeling. Methodology used to compute the peak <br />500-year flows was suggested and approved by the FEMA Region 8 contractor, Michael Baker, Jr. Ine. (Baker) (Jula <br />2004). <br /> <br />3.3 500- Year Flows <br /> <br />Section 3 <br />Hydrology <br /> <br />The 100-year storm hydrograph developed by Merrick (1983) was utilized in the CUHP model runs to generate the <br />hydrographs for the Master Plan, using a time step of 15-minutes (see Figure 3-5). The modeled hydrographs were <br />then input to the UDSWM model to route the flows in the South Platte River through the Study Area. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Baker suggested using the 500-year flow rate from the 1995 Adams County Flood Insurance Study (FIS) at the <br />confluence of the South Platte River with Todd Creek to calculate peak 500-year flows at other locations along the <br />South Platte River. The following formula was thus used to calculate 500-year flows: <br /> <br />QIOO, <br />-- <br /> <br />Q'OO,i-1 <br /> <br />3.2.3 Results <br /> <br />Simulated hydro graphs at selected locations for the 100-year storm event are shown in Figure 3-6. This figure <br />demonstrates both the progression and attenuation of the flood event as the flood wave traverses the Study Area. <br />At Franklin Street, the peak flow is approximately 21,500 cfs and is a result of the flood originating from upstream <br />of the Study Area. Below the confluences of Sand Creek and Clear Creek, the peak flow rises to nearly 40,800 cfs. <br />The peak flows begin to attenuate in the downstream direction, producing at l04th A venue a flow of 36,400 cfs and <br />at Henderson Road a flow of 32,200 cfs. The peak flow does not decrease any further downstream, remaining at <br />cfs at least until the downstream 45.000 <br /> <br />'I' <br /> <br />I <br /> <br />QSOO,i-1 <br /> <br />In the above formula, QSOO,i is the 500-year flow rate at cross-section i; Q500, i-I is the 500-year flow rate at the <br />downstream cross-section; Ql00,i is the 100-year flow rate at cross-section i, and Ql00, i-I is the 100-year flow rate at <br />the downstream cross-section. 500-year flows were developed for each model cross-section throughout the entire <br />Study Area, using Baker's methodology with the 1977/1985 FHAD 100-year flows that were used in the Master <br />Plan. Table 3-5 provides a summary comparison of 100- and 500-year flows. <br /> <br />Qsoo, <br /> <br />\1 <br /> <br />I <br /> <br />\1 <br /> <br />I <br /> <br />II <br /> <br />I <br /> <br />Cross- Master Plan FIS FHAO <br />Section 100-Year Q 500- Year Q 500- Year Q <br />10 Station (cfs) (cfs) (cts) Notes <br /> 32,500 57,500 57,500 US Hwy 85 <br />FISA 0+42 58,000 <br />10 128+66 33,600 59,446 Todd Creek inflow <br />29 426+14 35,400 62,631 120th Ave <br />FIS Z 451+00 <br />30 465+68 36,000 63,692 Bull Seep outfall <br />FISAE 600+20 <br />36 602+68 35,600 62,985 104th Ave <br />FISAI 710+30 <br />43 710+81 36,800 65,108 <br />FISAK 779+30 <br />45 779+41 37,200 65,815 88th Ave <br />FISAM 842+00 37,200 66,000 66,000 <br />50 854+73 37,200 66,000 UPRR Crossinq <br />53 887+50 37,600 66,710 Clear Creek <br />61.085 954+32 38,000 67,419 Sand Creek <br /> 22,300 35,000 39,565 15th Street <br /> <br />Table 3-5100/500-Year Flows <br /> <br /> <br />eonnuence wi CI_ ere.A: <br /> <br />00 0 0 0 0 0 0 0 0 0 0 6 b b b 6 0 b 6 6 6 0 0 0 0 0 0 0 <br />~ ~ ~ g ~ ~ ~ ~ ~ g ~ ~ ; ; ~ ~ ~ ~ ~ ~ g E ~ ~ ~ ~ ~ ~ <br /> <br />Time from Start of Storm Event (hours) <br /> <br /> 40,000 <br /> 35,000 <br /> 30,000 <br />~ <br />.2 25,000 <br />t <br />" <br />1: 20.000 <br />6 <br /> 15,000 <br /> Sase/Ill <br /> 10,000 <br /> .000 <br /> <br />Figure 3-7 presents the 1977/1985 FHAD <br />and modeled flow rates throughout the <br />study reach. The modeled flow rates <br />computed in this study are within plus or <br />minus 8 percent of the published <br />1977/1985 FHAD values. For the HEC-2 <br />modeling of existing conditions conducted <br />for the Master Plan, the 1977/1985 FHAD <br />peak flows were used, as these represent <br />the regulatory flows and their use <br />provides a direct comparison of modeled <br />flooding extent to that projected in the <br />1977/1985 FHAD studies. <br /> <br />32,200 <br />boundary of the Study Area. <br /> <br /> 197711985 FHAD 100-yr <br />. - . COM Model100-yr Tl <br />f ~ ~ ____1984 Phase A 2-yr ~ c ~ 2 <br />;;; . . . <br />c U U ~"'<~"= Interpolated 5-yr U . (; . <br /> . c <br />C ." . -4 ~ 1984 Phase A 10...yr i! ." ." ~ <br /> C C ." <br />E . . - .- 1984 Phase A SO-yr u: . 0 <br />~ l/) <; :to I- 1Il <br /> r-_ <br /> -- <br /> - <br /> -- <br /> - 4- _ _ _ _ _ _ _ . _ _ _ _ _ _ _ _ _ _. _._ _ _ _ _ _ _ _ _ _ _ _ __ <br /> -- <br />.....~ <br /> T-~.------------+-~._------- <br />- . ... <br />i . . 1 . ----f <br /> <br />Figure 3-6 <br />South Platte River <br />100- Year Hydrographs at Selected Locations <br /> <br />Simulated <br /> <br />60000 <br /> <br /><0000 <br /> <br />50000 <br /> <br />Also shown in Figure 3-7 are flow rates for <br />the 50-, 10-, 5-, and 2-year flood events. <br />The 50-, 10-, and 2-year events are as <br />reported in the 1984 Master Plan Phase A <br />Report (UDFCD 1984), The 5-year event <br />was estimated by interpolation between the <br />10-year and 2-year events. These flows <br />were define the <br /> <br />water surface <br />with the HEC- <br /> <br />used to <br />profiles and flooding extent <br />2 model <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Four locations that bracket the Study Area were identified along the South Platte with 500-year flow rates from the <br />Adams County, Weld County, and City and County of Denver FrS reports: 15th Street in Denver, Clear Creek, <br />Todd Creek, and U.S. Highway 85 near Evans. U.s. Highway 85, Clear Creek, and Todd Creek flows were used to <br />calculate 500-year flows at the model cross-sections. The 500-year flow at 15th Street was compared to the derived <br />results, and shows an approximately 4,600 cfs (13 percent) difference. As 15th Street is a considerable distance <br />upstream of the Study Area (approximately 3 miles), this difference was considered acceptable. <br /> <br />1000+00 800+00 600+00 400+00 200+00 0+00 <br /> Stationing from County Line (ft,) <br /> Figure 3-7 <br /> South Platte River <br /> 1 DO-Year Design Discharges <br /> <br />30000 <br /> <br />2lJOOO <br /> <br />10000 <br /> <br />o <br />1200+00 <br /> <br />~ <br />.!!. <br />GO <br />E' <br />'" <br />" <br />:;l <br />is <br /> <br />I <br /> <br />I <br /> <br />COlI <br /> <br />4/5/05 cJe <br /> <br />1 \40a92\PREP-FHAD\S3.DOC <br /> <br />06 <br /> <br />3-4 <br />