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<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.
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<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 />
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<br />QSOO,i-1
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<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.
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<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
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<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 />.!!.
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