Laserfiche WebLink
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Table 5. <br /> <br />Mean daily flows (cfs) and volumes (acre-feet) of the Green River for November, <br />1994 through March, 1995, as measured at Greendale, UT (USGS gage <br />09234500). <br /> <br />MONTH MINIMUM MAXIMUM MEAN VOLUME <br /> (acre-ft) <br />November 1994 820 1180 909 549,070 <br />December 1994 1290 1320 1305 80,250 <br />January 1995 1280 1310 1294 79,540 <br />February 1995 818 1310 1088 60,440 <br />March 1995 818 836 828 50,920 <br /> <br />Flow of the Green River at Jensen was supplemented by inflow of several tributaries, including the <br />Yampa River. Mean daily flows at Jensen varied from a high of 1,993 cfs in March to 1,319 cfs in <br />November (Table 6). The higher flows in March were the result of early spring runoff from the <br />Yampa River. <br /> <br />Table 6. <br /> <br />Mean daily flows (cfs) and volumes (acre-feet) of the Green River for November, <br />1994 through March, 1995, as measured at Jensen, UT (USGS gage 09261000). <br /> <br />MONTH MINIMUM MAXIMUM MEAN VOLUME <br /> (acre-ft) <br />November 1994 1180 1630 1319 78,510 <br />December 1994 1580 1850 1688 103,800 <br />January 1995 1530 1790 1675 103,000 <br />February 1995 1460 2440 1934 107,400 <br />March 1995 1460 2970 1993 122,500 <br /> <br />5.0 RIVER ICE CONDITIONS <br /> <br />Historically, an ice cap usually formed on the Green River in winter. For 18 years of record prior to <br />Flaming Gorge Dam, surface ice was reported on the river at Jensen during 1 to 5 months of each <br />year (Figure 4; U.S. Geological Survey Field Notebook, Data Courtesy of J. Schmidt, Utah State <br />University). Following completion of the dam in 1964, surface ice was reported during 1 to 4 months <br />in only 15 of 29 years. It appears that fluctuating releases of relatively warm hypolimnetic water in <br />winter have reduced the incidence of surface ice formation and increased the occurrence of jam and <br />frazil ice. These conditions may reduce the availability of backwater habitat in downstream nursery <br />areas of age-O Colorado squawfish. <br /> <br />11 <br />