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<br />Final Report <br /> <br />3-50 <br /> <br />September 2000 <br /> <br />and Labyrinth Canyons) or significant vertical accretion that has occurred in response to climatic <br />change (see Section 3.6.4). Very little floodplain habitat is available even at very high flows. <br /> <br />FLO Engineering Inc. (1996) modeled inundation of floodplain habitats in Canyonlands <br />National Park between RK 41 and 56 in Reach 3. Between 198 and 1,104 m3/s, little change in the <br />area of flooded habitat occurred. Between 1,104 and 1,500 m3/s, the amount of flooded habitat <br />increased from 2 to 200 ha(Figure 3.18). Another site in Reach 3 within Canyonlands National Park <br />was studied by C1uer and Hammack (1999). These authors used HEC-RAS (a numeric model <br />developed by the U.S. Army Corps of Engineers) to evaluate river-channel hydraulics for an 8-km <br />study site located between RK 61 and 69. They described the floodplain in this portion of Reach 3 <br />as a series of high, fairly continuous levees with basins and channels between the levees. At flows <br />between 509 and 1,924 m3/s, the amount of inundated floodplain would increase linearly from about <br />3 to about 130 ha. If existing levees were removed, the amount of inundated floodplain would <br />increase linearly from 23 to 162 ha over this same range of flows. <br /> <br />Floodplain inundation in Reach 1 is not required to meet life-history needs (e.g., growth and <br />conditioning habitat of larval fish) of any of the endangered fishes. Neither razorback sucker, <br />Colorado pikeminnow, nor humpback chub are found upstream of or within Browns Park (where <br />most floodplain habitats exist in Reach 1), nor are they expected to be found there because the cold <br />temperatures of the water prevent their use of these areas. Consequently, floodplain inundation in <br />Reach 1 is not an objective of the flow recommendations in this report. <br /> <br />3.7 SUMMARY OF RELATIONSHIPS BETWEEN FLOW, IN-CHANNEL <br />HABITATS, AND FLOODPLAIN INUNDATION <br /> <br />Table 3.14 presents a summary of flow patterns and levels that, on the basis of our current <br />understanding of the Green River system, would produce suitable habitat conditions for endangered <br />fishes in the Green River downstream of Flaming Gorge Dam. The flows identified are those that <br />have been demonstrated or estimated to restore dynamic hydrologic and geomorphologic processes <br />that would maintain those habitats in areas designated as critical habitat or areas occupied by the <br />endangered fishes. These flows are not the same for all portions of the river because tributary inputs <br />and geologic changes along the river affect flow levels, seasonal patterns, channel hydraulics, bed <br />characteristics, and sediment loads. Consequently, separate flow values are presented for each of the <br />three reaches. <br /> <br />The availability and suitability of low-velocity backwater habitats during the base-flow <br />period depend on flow, but their relationship to flow patterns and levels will change from year to year <br />as a function of the elevation of sediment deposits behind which these habitats form. Because these <br />elevations are set by preceding high flows and then eroded by subsequent flows, it is not possible to <br />recommend a single flow that will optimize habitat area in all years. A specific recommendation for <br />a given year would have to consider antecedent conditions, characteristics of in-channel sediment, <br />and existing channel morphology. <br />