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Last modified
7/14/2009 5:02:33 PM
Creation date
5/22/2009 4:57:14 PM
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UCREFRP
UCREFRP Catalog Number
8188
Author
Muth, R. T., et al.
Title
Flow and Temperature Recommendations for Endangered Fishes in the Green River Downstream of Flaming Forge Dam.
USFW Year
2000.
USFW - Doc Type
\
Copyright Material
NO
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<br />Filial Report <br /> <br />3-30 <br /> <br />September 2000 <br /> <br />Further attenuation in flow and stage occurs below Jensen, although this attenuation was <br />not modeled by Yin et al. (1995). Table 3.11 presents available measurements of flow and stage at <br />Jensen, Ouray, and Green River, Utah, and the release pattern of Flaming Gorge Dam during the <br />measurement period. Only measurements taken during periods of fluctuating releases from the dam <br />and during base-flow periods are presented. On the basis of these observations, one can conclude that <br />significant attenuation occurs between Jensen and Ouray and that any fluctuation effects are <br />essentially eliminated by Green River, Utah. This result is to be expected because the Green River <br />near Ouray is wide and unconfined, with a low gradient (0.0004). <br /> <br />3.5 GREEN RIVER WATER TEMPERATURES <br /> <br />Water temperature, particularly as it relates to habitat suitability in the critical summer <br />nursery period and to ice conditions in the winter, is an extremely important variable relating to <br />endangered fish populations. The Service began a program of monitoring river temperatures on the <br />Yampa and Green Rivers in 1987 (Smith 1997). Thermographs were placed at key locations on the <br />Yampa and Green Rivers (Table 3.12). Data from these thermographs, USGS gage data, and results <br />from work done by others are the basis for this section's description of the thermal regime of the <br />Green Ri ver. <br /> <br />Winter snows accumulate in the Green River basin from October through mid-April. When <br />air temperatures in the basin begin to rise in March and April, snowmelt and runoff begin. As flow <br />increases, the cold water gets warmer as a result of interactions with the channel bed, the <br />atmosphere, and direct solar radiation. Figure 3.14 compares water temperature at five locations <br />downstream from Flaming Gorge Dam along the Green River during June through September 1996. <br />This figure illustrates the warming that occurs downstream of Flaming Gorge Dam. <br /> <br />Table 3.11.-Measured within-day flow and stage changes for the Green River at USGS <br />stream gages near Jensen, Ouray, and Green River, Utah, under different Flaming Gorge Dam <br />operations. <br /> <br /> Flaming Gorge Release (m3/s) Stage Change (m) <br />Date Minimum Maximum Jensen Ouray Green River <br />Oct 7,1987 23 71 not available 0.11 not available <br />Nov 11, 1993 23 120 0.38 not available 0.02 <br />Nov 9,1998 52 84 0.13 0.05 0.00 <br />Nov 17, 1998 40 121 0.31 0.12 0.01 <br />
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