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FLOOD10395 (2)
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Last modified
11/23/2009 12:53:28 PM
Creation date
7/26/2007 11:37:10 AM
Metadata
Fields
Template:
Floodplain Documents
County
Montezuma
Community
Dolores
Stream Name
Dolores River
Title
Dolores River near Dolores, Colorado, Flood Insurance Study
Date
5/1/2004
Prepared For
Dolores
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />, <br /> <br />e Table 10 <br />" User Gage Weighting, 5-6 September 1970 <br />" <br /> , Most Upstream to McPhee Dam <br /> Precipitation (inches) <br /> Subbasin Drainage Area Depth <br /> Name (sq mi) (inches) <br /> West Fork Dolores 168 3.0 <br /> Dolores Headwaters 105 3.2 <br /> Dolores Upper Mid 65 2.2 <br /> Bear Creek 34 2.3 <br /> Dolores Mid 74 3.0 <br /> Dolores Lower 57 2.2 <br /> Dolores Out 1 2.2 <br /> Lost Canyon Creek 71 3.0 , <br /> " <br /> Lost Canyon Creek Out 3 2.5 <br /> Dolores Lower Out 1 2.3 <br /> I <br /> 6.9 Model Validation for Flood Simulation. The validity of the upper Dolores River <br /> <br />basin HMS model developed for this flood insurance study was tested by using it to reproduce the <br /> <br />September 1970 high flow event on the watershed. The HMS model was run for the 1970 storm, <br /> <br />e <br /> <br />using the subbasins, unit hydro graphs, loss rates, baseflow, Muskingum routing parameters, 2-day <br /> <br />storm isohyetal map and hourly precipitation distribution discussed above. A comparison <br /> <br />between the output "computed hydro graph" and the observed hydro graph for the 1970 flood at <br /> <br />the Dolores gage is presented graphically on Plate 10. The two hydro graphs are tabulated in <br /> <br />Appendix A, Table 4. Since an observed hourly hydro graph for the East Fork below Rico gage <br /> <br />was not available for comparison, the peak flow and three-day volume were compared. Table 11 <br /> <br />presents a comparison of computed and observed peak flows and volumes at the Rico and Dolores <br /> <br />gages. The September 1970 rainflood peak at Dolores was about a 4% event. The unit <br /> <br />hydro graph and streamflow routing parameters used for the 1970 flood calibration were not <br /> <br />changed for the 1 % rainflood simulation because a change in the results would be negligible. The <br /> <br />HMS model is assumed suitable for computing 1 % chance flood hydro graphs for this study. <br /> <br />e, <br /> <br />23 <br />
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