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<br />8 <br /> <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 />regimes. These contrasting conditions provided an excellent opportunity to examine fish <br /> <br /> <br />response to different winters under similar dam operation. <br /> <br /> <br />Winter 1 (1986.87). Higher than normal air temperatures in Winter 1 produced <br /> <br /> <br />above normal water temperatures near Jensen. Monthly maximum air temperatures for <br /> <br /> <br />December through March were from 0.7 to 4.10C above normal, while minimum <br /> <br /> <br />temperatures were 1.2 to 6.10C above normal. Monthly water temperatures were up to <br /> <br /> <br />2.30C warmer in February of Winter 1 than in Winter 2 (Figure 7). Higher releases from <br /> <br /> <br />Flaming Gorge Dam in Winter 1 also moderated river temperatures by delivering a larger <br /> <br /> <br />thermal mass to downstream areas. <br /> <br /> <br />Ice formation in Winter 1 was minimal and temporary, except for the lower 20 miles <br /> <br /> <br />(RM 270-250) of the study area, where surface ice persisted for about 3 weeks, from mid <br /> <br /> <br />to late January, 1987. This surface ice thickened to 3 to 5 cm, and was broken and <br /> <br /> <br />transported downstream by large mainstem fluctuations. Otherwise, surface ice persisted on <br /> <br /> <br />backwaters and along some shorelines from mid-January through February, 1987. These thin <br /> <br /> <br />ice layers extended from shorelines and backwaters in the morning, and usually melted as <br /> <br /> <br />the main channel warmed during the day. Jam ice was observed on the Green River for <br /> <br /> <br />only a short period in Winter 1, between mid-January and mid-February. Frazil ice was also <br /> <br /> <br />rare in Winter 1, forming at night during low temperatures, and melting from daytime solar <br /> <br /> <br />radiation. Although the Green River did not freeze above Jensen during Winter 1, the <br /> <br /> <br />Yampa River was frozen much of the winter. Breakup of the Yampa River contributed to <br /> <br /> <br />heavy ice flows in the Green River on March 9-10, 1987. <br />