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5 RECOMMENDATIONS <br />1. To prevent ice breakup, or the transport and deposition of frazil ice in areas used by <br />overwintering endangered fishes, large daily fluctuations at the Jensen gage should be <br />avoided during extremely cold weather (mean daily air temperature about -7 'C or <br />below) until surface ice has formed to approximately RM 310. During milder winters, <br />when frazil ice production is reduced, less restrictive operations could occur without <br />depositing frazil ice under the ice cover and without breaking up all but the thinnest ice <br />covers past about RM 300 (Jensen Bridge). During the 1997 field study the mean daily <br />flow at the Jensen gage was approximately 2,440 cfs and fluctuated daily between 1,700 <br />and 3,500 cfs. These fluctuations did not deposit significant amounts of frazil under the <br />ice cover and did not break up the ice cover downstream of RM 306. <br />2. Collect accurate hourly water temperatures at a number of locations throughout the study <br />reach to improve calibration of the ice-process model and to test specific assumptions in <br />the model (e.g., timing of the formation of frazil ice). To accomplish this, measurements <br />accurate to the nearest 0.1 °C would be useful. Additional temperature information would <br />provide information about the environmental conditions (such as supercooled water) that <br />endangered fishes may encounter within the study reach. Collection of temperature data <br />in other portions of the river could be used to investigate the distance to which Flaming <br />Gorge Dam exerts a thermal influence on the river and the effects of fluctuating flows on <br />temperature regimes. <br />3. Additional investigations should be conducted to characterize winter conditions in <br />backwaters and other low-velocity habitats that may serve as overwintering areas for <br />juvenile endangered fishes. Although such studies were conducted in backwater areas by <br />Valdez and Cowdell (1999), the winters during those studies were unusually mild. <br />Although main channel ice processes in the principal area used by overwintering native <br />fishes do not appear to be greatly affected by fluctuating flows, shallower backwater <br />areas used as nursery habitats by age-0 fish may be susceptible to inundation and <br />desiccation. Consequently, the degree of use of these areas during winter and the <br />physical conditions within such areas should be examined. <br />-27-