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<br />II <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />!I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />. <br /> <br />I <br /> <br />I <br /> <br />! . <br /> <br />I <br /> <br />Table 6. Peak Discharges Along Pawnee Creek Main Channel Under Existing Conditions <br /> <br />Location 10-Year 50- Y ear 100-Year <br /> (cfs) (cfs) (cfs) <br />*Mouth (South Platte River 100- Y ear Floodplain) 1517 2026 2226 <br />*Upstream HWY 6 1517 2026 2226 <br />*Upstream CR. 33 2945 5434 6645 <br />*Upstream CR. 31 3264 6729 8611 <br /> <br />* Split flows depicted in Figure 8A cause reduced discharge in the main channel <br /> <br />There are several areas where the flood flows exceed the capacity of the channel for the 10-year, 50- <br />year, and 100-year events. Flows which split from the main channel are subtracted out and are <br />accounted for under existing conditions; therefore, the discharges vary significantly from downstream <br />to upstream. For Pawnee Creek Overflow in the City of Sterling, 100-year flows are estimated to be <br />5,000 cfs, <br /> <br />As a result ofthe improvements proposed in this report, flood flows are contained in the areas adjacent <br />to the channel in the north overbank. Therefore, these flows were considered a part of the main <br />channel and were included in the analysis. Improvements were not proposed in the upper reaches of <br />Pawnee Creek along the south overbank since they do not directly contribute to the Pawnee Creek <br />Overflow in the City of Sterling, Subsequently, the areas where flows split out of the channel and <br />travel southwest towards the Town of Atwood were considered valid for proposed conditions and were <br />subtracted out of the main channel at these locations, A portion of these flows eventually drain back to <br />the main channel at HWY 6 and the Pawnee Creek crossing, <br /> <br />A field survey was completed by the Colorado Water Conservation Board in the area along HWY 6 <br />south of Pawnee Creek to determine the amount of flows which gets back to the main channel. The <br />flows in this area are controlled by an existing berm which blocks the flow path. Estimates were made <br />by the Colorado Water Conservation Board as to how much of the flow overtops the berm and how <br />much would be forced over HWY 6 and the UPRR embankment. Flows expected to overtop the berm <br />were added into the main channel at the HWY 6 bridge crossing of Pawnee Creek. A swnmary of the <br />discharges used for developing the proposed improvements are presented in Table 7. <br /> <br />Table 7. Peak Discharges Along Pawnee Creek Main Channel Under Improved Conditions <br /> <br />Location 10- Y ear 50- Year 100-Year <br /> (cfs) (cfs) (cfS) <br />Mouth (South Platte River 100- Y ear Floodplain) 3800 6500 8200 <br />Upstream HWY 6 3800 6500 8200 <br />Upstream CR. 33 2945 5434 6645 <br />Upstream CR, 31 3264 6729 8611 <br /> <br />The discharges presented in Tables 6 and 7 were used in the hydraulic analysis to develop flood water <br />surface elevations for the different scenarios that were studied. Figure 8A presents a diagram of the <br />peak discharges and flow splits along Pawnee Creek <br /> <br />25 <br />