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<br />evenly-spaced sites. Global models were built; best-fit models had the highest RZ and the fewest <br />number of parameters. <br />The model developed for the Green River in lower Browns Park was used for two <br />additional purposes. First, daily summer water temperature predictions for the 1992-1996 period <br />were estimated using annual air and discharge measurements as independent variables. Accuracy <br />of model predictions for each year was determined by comparing independent observations of <br />daily water temperature (G. Smith, USFWS, unpublished data) collected about 10 km upstream <br />at BPNWR. Water temperatures averaged 0.8°C cooler there than at lower Browns Park in the <br />summers of 1994 and 1995. Therefore, that value was added to BPNWR observations in all <br />years to make comparisons with lower Browns Park model predictions realistic. <br />Another purpose of the lower Browns Park model was to predict water temperatures <br />under high (50 m3/s), moderate (37.5 m3/s), and low summer base flows (25 m3/s). This site was <br />chosen because it is upstream from where most native and endangered fishes were thought to <br />occur. In all scenarios, flow declined from high levels in early-June to 50 m3/s by 1 July and, in <br />the high base flow scenario, remained at that level for the remainder of the summer. In moderate <br />and low flow scenarios, target base flow was achieved by 15 July. Those base flow scenarios <br />were within the summer discharge range used to construct the model and represented realistic <br />operational scenarios for water levels discharged from Flaming Gorge Dam from 1992 to 1996. <br />Mean daily air temperature for the period of record at BPNWR was the other independent <br />variable. Predicted and observed water temperatures and discharge regimes for the Green River <br />at lower Browns Park were compared with similar observations for the unregulated Yampa River <br />where a reproducing population of Colorado pikeminnow existed (Bestgen et al. 1998). <br />Predicted water temperatures were compared among all three models to understand <br />temperature levels and warming rates of the Green River under different summer discharge <br />regimes. In those scenarios, air temperature was held at a constant 19.3°C, the mean daily <br />average from June through August over the period of record (N. Doesken, Dept. of Atmospheric <br />Science, Colorado State Univ., unpublished data). <br />11 <br />