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,Tia Juana Bottom <br />Calibration work on the last section of the model from Ouray <br />Refuge to Tia Juana Bottom began in June of 1988, after the <br />completion of the collection of data to build a rating table. <br />The time period selected for the calibration was July and August <br />1987. This period was selected because it represents a time when <br />a series of controlled releases were being made from Flaming <br />Gorge. Starting on July 6, 1987, a beginning release of 2100 cfs <br />was established. This release was held constant, allowing flows <br />at Jensen, Utah to stabilize and only vary 100-200 cfs depending <br />upon the flow of the Yampa River. In successive weeks, releases <br />from the dam were decreased to 1800 cfs, 1500 cfs, 1300 cfs, <br />1,000 cfs, and 800 cfs. In mid-August, peaking power releases <br />were resumed and a release pattern of 1200 cfs to 2600 cfs was <br />established. <br />During this period, numerous biological sampling and backwater <br />mapping research projects were in progress all along the Green <br />River, from the dam down to Willow Creek. Each of these studies <br />needed to be correlated to flow information at a specific time <br />and location; unfortunately, the only information available was <br />the Jensen USGS gage. Based upon request for flow information at <br />other locations, SSARR was set up and calibrated for the test <br />release period. <br />The set up of SSARR down to Tia Juana Bottom was accomplished by <br />requesting release information from Flaming Gorge. This <br />information was provided by the Western Area Power <br />Administration, who provided hourly power production at Flaming <br />Gorge in megawatts. The megawatts information was converted to <br />cfs by multiplying megawatts by 32. This conversion factor was <br />supplied by the Bureau and is based upon various rating and head <br />factors unique to the Flaming Gorge dam and powerplant. <br />Next, hourly flow information at Deerlodge Park on the Yampa, <br />Jensen on the Green River, Randlett on the Duchesne River, and <br />Watson on the White River was requested from the USGS. This <br />information was then keypunched and reformatted for SSARR model <br />input. The final step was the set up of the SSARR model network <br />and building the input data file. <br />The extended network included computational nodes at the Green- <br />Duchesne confluence, the Green-White confluence, and Tia Juana <br />Bottom. Nodes were later added to represent gaged locations on <br />the Duchesne and White Rivers. These reaches were found to be <br />necessary to accurately control the time at which water arrived <br />at Tia Juana Bottom. Without these reaches water arrived <br />instantaneously and precluded any accurate calibration. <br />Calibration of the model was accomplished using the following <br />data recorded July 1, 1988 through August 31, 1988: Flaming <br />Gorge releases, flow of the Yampa, recorded flow at Jensen, <br />Duchesne and White River flows and recorded flow at Tia Juana <br />Bottom. <br />14