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<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 />5. <br /> <br />2. <br /> <br />their historic operating practices, or other arrangements made for providing <br />flood storage, then the hydrology downstream would be lower, <br /> <br />cfV'b,,^'<'-fkZ^<\ <br />The raillin~to the Moffatt Tunnel provides, we believe, significant flood <br />storage on the south tributaries from the foothills to above Gross Reservoir. <br />We are familiar in detail with one site on South Draw where about 80 to 100 <br />acye:teet of, sto.~age olccurs and reduces the 100-year flood pe~k by morEj . <br />than hal1 0:.\ ~ <,(,,,\'1,,,. c~ /' / ^ J-6."",Jd'l'l <br />,0. "^" ~ ~'IW / r"'^3-'l v <br />There may be as many/a's 20 to 30 storage~ that exisy{ that ~ from very <br />small to sizes such asilsouth Draw. Since agreemeQts are not in placlt to <br />sustain these storages, they have not been includecf These storage~xist, <br />benefitting the downstream conditions for most events, but also maypresent <br />hazard as the storages are not engineered for flood control and may be <br />susceptible to breeching. <br /> <br />3. <br /> <br />When flood control facilities, floodplain mapping, or refined surveys are <br />available the hydrology model can be further refined to better depict flow <br />splits and hydraulic controls. The 500-year flood model prediction requires <br />further review to confirm flow splits and patterns. Thus, we can envision <br />further revisions to the hydrology model in the future. <br /> <br />4. <br /> <br />The UDSWMM program has very limited stream flow routing algorithms. We <br />feel it is inadequate to simulate the dynamic floodplain storage routing of the <br />South Boulder Creek below Eldorado Springs and the West Valley Overflow. <br />Thus the flows depicted in these areas shown in the present draft modeling <br />are probably high. Effectively the peaks of the hydrographs are "trimmed" <br />and sent to the West Valley Overflow without the natural attenuation that <br />exists. <br /> <br /> <br />Our limited sensitivity tests indicate that the model is highly responsive to <br />the geometry given for the South Boulder Creek main stream. While our <br />work for the Colorado State Park has afforded the opportunity to incorporate <br />field surye~ of representative sections at Eldorado State Park, it may be <br />worthw~~to conduct field surveys of representative se~' ns at other <br />locations in order to better represent the mountain strea s. ) <br />,.,,/ <br /> <br />RECOMMENDATIONS <br /> <br />1 . The results are reasonable to begin a review and refinement by independent <br />experts and the sponsors, <br /> <br />2. The results are reasonable to begin the alternative evaluation process. <br />Alternatives developed might consider options to "firm up" existing flood <br /> <br />1- 15 <br />