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<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 /> <br />historic flows can jeopardize those species. The importance of flow maintenance to the <br /> <br />. ed Colorado River fishes is recognized throughout the Colorado River Basin (Stanford <br />ff; ::ir <br />IJJ24;),;lfr <br /> <br />In the lower basin, flow regulation and habitat fragmentation have extensively altered <br />most riverine habitats, leaving few historic riverine habitats in tact (Marsh and Minckley 1985, <br />Minckley 1985). In the upper basin, flow regulation has generally reduced the peak of spring <br />runoff and increased the magnitude of base flows in historic habitat. Since 1950, annual peak <br />discharge of the u olorado River has decreased by 29-38% (Van Steeter and Pitlick 1998) <br />in occupied habitat ... Grand Valley. Flows of the Green River near Jensen, Utah, have <br />'i:;~ <br /> <br />decreased by 13-35 o.d~ng spring and increased by 10-140% during summer and winter due to <br />regulation by Flaming Gorge Dam (Muth et a1. 2000). Overall, storage of spring flows have <br />reduced spring runoff by 28% in the Green River and by 37% in the Colorado River during May <br />and June (USGS flow records, 1906-1982). The effect of these flow modifications on the <br />endangered fishes is not clear, but a sudden and dramatic decline occurred in the Green River <br />shortly after completion of Flaming Gor am in 1963 (Vanicek 1967, Vanicek and Kramer <br />1969). It is hypothesized that stream ification reduced high-velocity flows that flush <br />sediments from spawning cobbles (Van Steeter and Pitlick 1998), reduced channel and habitat <br />complexity with concomitant losses in food production (Osmundson 1999), and reduced the <br />availability of flooded bottomlands during spring runoff, which are possibly used as nursery <br />habitats by newly-hatched larvae and young. <br />Streamflow modification in the Colorado River Basi esulted in depleted flow and <br />altered flow regimes. These changes have altered water tern e, sediment loads, water <br />quality, and habitat (see Section 3.1.1.2). Flow regulation is attributed primarily to dam <br />operations, irrigation diversions, transbasin diversions, riverside pumps, and instream industrial <br />and municipal pumping systems. In the lower basin, most of the main channel has been <br />extensively fragmented with dams and diversions, and there are few remaining riverine reaches. <br />In the upper basin, streamflow regulation has affected most of the remaining riverine habitat, and <br />little flexibility remains for reoperation of existing dams to provide flows to assist rec <br />Colorado River endangered fishes. <br /> <br /> <br />11 <br />