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<br />'001309 <br /> <br />. <br /> <br />. <br /> <br />Draft Task 9 Technical Memorandum <br /> <br />Refinement of Stagecoach Reservoir Inflows <br /> <br />Model inflows to Stagecoach Reservoir were developed in a manner similar to the <br />methods used to develop Elkhead Reservoir inflows, This method is summarized as follows: <br /> <br />1. Assemble data for USGS gage 9237500. The period of record for <br />this gage is 1940 to 1944 and from 1957 to 1988. The gage was <br />extended by regression against the Steamboat Springs gage on the <br />Yampa River to cover the entire 53 year study period between 1930 <br />and 1982. In 1989 Stagecoach Reservoir was completed and a new <br />gage (9237450) was installed immediately upstream of the reservoir. <br />The regression equation used to extend the record of gage 9237500 <br />was: <br /> <br />Annual Discharge Annual Discharge <br />Gage 9237500 extension: Gage 9237500 = 0.2521 * (Gage 9239500) - 17444 <br /> <br />R2 = 0.889 <br />Average Annual Error = 1.11 % <br /> <br />The estimated average annual flow at the site of the Stagecoach <br />Reservoir dam is 62,077 af. <br /> <br />2. The estimated average annual yield was disaggregated into monthly <br />flows using the average monthly distribution over the period of record <br />for gage 9237500. <br /> <br />3. Because gage 9237500 is located very close to the location of the <br />Stagecoach dam it was not necessary to transpose the gage data <br />upstream or downstream. <br /> <br />In addition to numerous irrigation ditches there are several small reservoirs located <br />above Stagecoach Reservoir which affect the natural hydrology of the Yampa River. Included <br />are Stillwater Reservoir and Yamcolo Reservoir. In developing the inflows used in the basin <br />model an assumption was made that these ditches and reservoirs would continue to operate as <br />they have historically and will continue to result in a similar pattern and amount of net <br />depletion to the basin. <br /> <br />There has been recent speculation that depletions above Stagecoach Reservoir are <br />increasing and that the historical inflows may over-represent future inflows. While recent gage <br />data (9237450) show lower inflows, the period of record is very short and covers only <br />relatively dry years. This issue has been discussed with Division 6 staff, however a defensible <br />alternative for estimating Stagecoach Reservoir inflows has not been developed. Continued <br />monitoring of Stagecoach inflows in the future may reveal more about this issue. <br /> <br />The Upper Yampa Water Conservancy District has investigated the possibility of <br />supplementing inflows to Stagecoach Reservoir by means ofa diversion from Morrison Creek <br />into the Little Morrison Creek drainage and then into the reservoir. To date this plan has not <br />been developed. Morrison Creek is a tributary flowing into the Yampa River at a point just <br />below Stagecoach Dam. The average annual yield of Morrison Creek is approximately 59,000 <br /> <br />5 <br /> <br />Iii: ~;,~ <br />