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<br />Final Report <br /> 1200 <br /> 1100 <br /> 1000 <br />- <br />~ 900 <br />C') <br />E 800 <br />- <br />'" <br />== 700 <br />0 <br />u: 600 <br />~ <br />as <br />CD 500 <br />0.. <br />C'I 400 <br />s::: <br />'i: <br />C. 300 <br />en <br /> 200 <br /> 100 <br /> 0 <br /> <br />3-13 <br /> <br />September 2000 <br /> <br />IliI Vampa River <br />. Green River above Vampa <br /> <br />Flaming Gorge Dam <br />Completed <br /> <br /> <br />~ 0 N ~ ID ~ 0 N ~ ID ~ 0 N ~ ID ~ 0 N ~ ID ~ 0 N ~ ID <br />~ m m m m m ID ID ID ID ID ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ m m m m <br />m m m m m m m m m m m m m m m m m m m m m m m m m <br />~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ <br /> <br />Figure 3.5.-Contributions of the upper Green River and Yampa River to spring peak flows <br />at the USGS stream gage near Jensen, Utah, 1947-1996. <br /> <br />relative contribution of the upper Green River to the peak flow decreased. For the period of 1947 to <br />1962, the mean annual peak at Jensen was 680 m3/s. Since 1963, the mean annual peak has been <br />reduced to 493 m3/s (FLO Engineering, Inc. 1997). Despite this reduction in the mean annual peak <br />flow, the highest peak on record at Jensen (1,133 m3/s) occurred on 18 May 1984. The lowest annual <br />peak on record at Jensen was 201 m3/s on 26 April 1989. <br /> <br />This natural year-to-year variability in flows makes it difficult to make pre- and post-dam <br />comparisons to illustrate the effects of Flaming Gorge Dam operations on flows. To understand the <br />effects of operations, a simulated time series of daily unregulated flow was developed for this report <br />(see Appendix A for a description ofthe approach used) and compared with gauged flow data during <br />the same period. Unregulated flows for the period 1963 to 1996 were generated by using numeric <br />modeling techniques in which the effects on flows from operating Flaming Gorge and Fontenelle <br />Dams were removed and propagated to the Greendale, Jensen, and Green River gages. These <br />modeled unregulated flows are used in this section to characterize the hydrology of the upper Green <br />River basin and quantify effects of dam operations on Green River flows. <br />