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The evaluation of flow in the study reach during the winter was based upon records from <br />the Jensen gage (USGS Station No. 09261000), located approximately 93 river miles <br />downstream of the dam at RM 316.6, in the upstream end of the study reach. There is a nearly <br />continuous record for this gaging station for the period from October 1946 to the present. <br />2.2.2 Water and Air Temperature Measurements <br />Periodic water temperature measurements of the Green River have been made by the <br />USGS at their Jensen gage site. Measurements of the temperature of water released from <br />Flaming Gorge Dam were also available for some years. Maximum and minimum daily air <br />temperature measurements were obtained from three weather recording stations in the vicinity of <br />the study reach: 1) Dinosaur Quarry in Dinosaur National Monument, 2) Vernal, Utah, and 3) the <br />Ouray National Wildlife Refuge. The air temperature measurements from these sites were <br />similar, differing by only about 0.6°C on any given day. For the purposes of this, study, it was <br />decided to use the Vernal, Utah air temperature records, which were more extensive and <br />complete than for the other recording stations. The daily average air temperature was estimated <br />for each day by taking the average of the maximum and minimum temperature reported for each <br />day (Panofsky and Brier 1968). <br />A good index of the severity of a winter can be calculated by totaling the number of <br />freezing degree days ("accumulated freezing degree days", abbreviated AFDD) throughout the <br />winter period. The number of freezing degree days that occur on any day is found by subtracting <br />the daily average air temperature from 0°C. For example, if the daily average temperature is <br />-5 °C, the number of freezing degree days for that day would be 5. If the daily average <br />temperature is above 0 °C, a negative number of freezing degree days is found for that day. The <br />severity and length of winters in the study area were determined for each year from 1950 through <br />1997 by finding maximum AFDD for each winter period and by determining the date on which <br />the maximum AFDD value occurred. <br />2.2.3 Historical Ice Observations <br />There are only a limited number of historical ice observations available for the Green <br />River in the vicinity of the study area. These include a summary of USGS observations made at <br />irregular times throughout the winter2, and the BIO/WEST reports of Valdez and Masslich <br />(1989) and Valdez and Cowdell (1999). <br />2The summary of USGS observations was based upon information in unpublished USGS logbooks <br />obtained in 1992 by Dr. Jack Schmidt, University of Utah. <br />-7-