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STIIDY AREA <br />Sampling was conducted in a 16.1 km reach of the Green River wholly with <br />boundaries of Ouray National Wildlife Refuge (NWR) (Figure 1). The reach incl <br />riverine habitat between the upstream portion of Leota Bottom (river kilometer <br />the inlet to Woods Bottom (RK 405.5). This portion of the Green River is char <br />extremely low gradient and slow flow. River bed sediments consist of sand, mu <br />Eleven island/sandbar complexes and eleven perennial sandbar complexes ars pre <br />reach. Many migrating sandbars develop each year. Deposition and erosion of <br />form numerous backwater habitats in this reach. Backwaters are formed most co <br />through sand wave migration and scouring. <br />Habitat conditions in this reach are determined by annual flows. Deposi <br />spring peak flows is determined largely by output of the Yampa River and Flami <br />Spring high flows of up to 23,000 cfs were observed. Sculpting of aggraded ma <br />upon summer and winter flows. Summer flows during the study were fairly stabl <br />depending upon the year, were between 1400 cfs and 2000 cfs. Winter flows var <br />high as 4000 cfs. Main channel temperatures varied with annual weather Condit <br />seasonality. Spring temperatures from 4°C to 12°C, summer temperatures from 2 <br />and fall temperatures from 10°C to 20°C were observed. <br />Islands and shoreline areas are dominated by cottonwood (Populus freemon <br />dense understory of salt cedar (Tamarix ramosissima), willow (Sa1ix exigua, S. <br />an-ygdaloides) and skunkbush sumac (Rhus trilobata). Forb and grass communitie <br />