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INTRODUCTION <br />Background <br />The U.S. National Park Service has del <br />hydrograph for the continued preservation <br />processes of the Yampa River in Dinosaur <br />related biological and channel morphologic <br />streamflow hydrograph was derived primarily <br />the sediment transport balance in the Yampa <br />simulated hydrograph is appropriate for th <br />aquatic species, a computer simulation of t <br />reduced discharges was conducted. The U.S <br />Flow Group (IFG) water temperature computer <br />to the Yampa River for six historical year <br />cold, average, and hot climatic years <br />compiled for input to the model. The r <br />temperature as a function of discharge. <br />eloped a minimum streamflow <br />of natural conditions and <br />National Monument and its <br />al resources. This minimum <br />on the basis of sustaining <br />Canyon. To ensure that this <br />biological functions of the <br />e water temperatures for the <br />Fish and Wildlife Instream <br />simulation model was applied <br />of flow record. Relatively <br />f meteorological data were <br />cults show the variation in <br />Objectives <br />The purpose of this study is to de <br />temperature of the Yampa River in Dinos <br />possible reduction in the water discharge <br />through an analysis of historical flows. <br />squawfish, which spawns in the Yampa Can <br />mately river mile 16.5 to 20.5, require <br />corresponding to certain discharges to enst <br />response. The National Park Service (NPS) <br />(O'Brien, 1984) was examined to determine <br />ing historical observed water 'temperatu <br />objectives were outlined to conduct the w <br />the Yampa and Green Rivers in Dinosaur Nat' <br />ermine the effects on water <br />ur National Monument from a <br />This study is accomplished <br />Specifically, the Colorado <br />ron in a reach from approxi- <br />s certain water temperatures <br />re a proper spawning behavior <br />minimum streamflow hydrograph <br />its suitability for duplicat- <br />es. The following specific <br />ter temperature simulation of <br />onal Monument. <br />1) Collect and prepare, as input o the model, meteorological, <br />topographical and channel geometry data f r the Yampa and Green Rivers <br />in the northwest Colorado area. ;Six years of data, representing a range <br />of relatively cold, average, and hot climatic years were chosen for <br />simulation of the period between March 1 nd August 15. <br />2) Construct and arrange data fi es in the proper format for <br />input to the IFG temperature model to si ulate water temperatures on a <br />weekly basis. <br />3) Calibrate the model for the <br />4) Simulate the water temperaturE <br />the NPS minimum streamflow hydrograph an <br />compare with the historical water tempera <br />storical water temperatures. <br />for composite hydrographs of <br />the historical discharges and <br />res.