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<br />FINAL REPORT, November 2003 <br />High-jlow Requirements for the Duchesne River <br /> <br />Reconstruction of the 20th century geomorphic history of the lower Duchesne River allows <br />us to characterize the unique responses of this system to historical fluctuations in discharge and <br />sediment supply, and to identify the key geomorphic components controlling those responses. <br />This information enables us to predict future channel changes with a greater degree of <br />confidence. In addition, an historical perspective is necessary to evaluate the current trajectory <br />of channel change and address the question as to whether the channel is currently adjusted to the <br />prevailing hydrologic conditions. <br /> <br />4 <br />