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<br />001883 <br /> <br />projected impacts of coal-resource and associated economic development on the re- <br />gional water resources of the Yampa River basIn (Steele and others, 1976a; 1976b). <br /> <br />An extension of the multi reservoir-flow model section of this report recently <br />has been completed by Veenhuis and Hi 11 ier (1982). The extended work principally <br />'shows effects of additional variations of water use for the proposed agricultural <br />and transmountain diversions with some reservoir configurations as given in this <br />report. The Veenhuis and Hill ier (1982) study, by simulating the different degrees <br />of development, provides a greater range of alternatives for basin managers or <br />planners to consider. <br /> <br />The techniques and procedures used in the model-analysis sections of this <br />report are presented in considerable detail so that the appl icability to other <br />river basins can be determined. Results of this report, however, are summarized in <br />less detail for the planner or declsionmaker in a Phase-I I summary report (Steele <br />and Hillier, 1981). <br /> <br />Appreciation is extended to the following individuals who contributed to the <br />study: D. B. Tramberg, appl ication and calIbration of the dissolved-sol ids model <br />developed by the U.S. Bureau of Reclamation; T. L. Washington, data coding; and <br />S. M. Hofford, data processing and modeling application. <br /> <br />MODEL DESCRIPTIONS <br /> <br />The computer models used in this study were selected from several available <br />operational models. Some of the guidel ines of the model-selection procedure used <br />for this study are defined by Jennings and others (1976). The choice of these <br />three particuiar models is not an endorsement because other mrdels also could have <br />been used. The multi reservoir-flow model chosen was the HEC-3 streamflow-routing <br />model developed by the U.S. Army, Corps of Engineers (1968) and uses techniques <br />discussed by Rutter and Engstrom (1964). The dissolved-sol ids model chosen waS <br />the NWOl river-salinity routing model developed by the U.S. Bureau of Reclamation <br />(Rlbbens, 1975). The single-reservoir model chosen was an adaptation (Adams, .1974) <br />of the reservoir-stratification and concentration-prediction model developed at <br />the Massachusetts Institute of Technology (Markofsky and Harleman, 1971). <br /> <br />The multi reservoir-flow model was developed to perform multipurpose, multi- <br />reservoir routings of streamflow in a river basin. The Yampa River basin was <br />depicted in the model by designating control points at reservoirs, diversions, re- <br />turn flows, and strea.m confluences. Monthly incremental runoff (runoff occurring <br />between a control point and any control points immediately upstream) was specified <br />for each control point. The total streamflow was then computed at each control <br />point by summing the upstream incremental runoff values. Monthly diversions or re- <br />turn flows were specified for the appropriate control points. For each reservoir, <br />monthly evaporation rates, outflow capacity, area-capacity curves, and the operat- <br />ing rules were specified. Operating rules were entered into the model by using six <br /> <br />4 <br /> <br />,,-,,' <br /> <br />;-X;i-:' <br /> <br />;~:: <br /> <br />I <br /> <br />y.::: <br /> <br />.' ~..:' , <br /> <br />~~>~ <br />):';1 <br />"..' <br />.:,:.;.; <br />:>', . <br /> <br />~. ">;<..- <br />-~:;:::-~': <br />,',. <br />~{iF} <br />,",;:':~'. <br />;(;? <br />" r.::;\~) <br />I <br />@~ <br />'~3l <br />:~t::~.; <br /> <br /> <br />~ <br />~ <br /> <br />~;f.~~ <br /> <br />I <br /> <br />'''~ <br />~tt <br />/t~:1 <br />....,.,. <br />". .,>~,. <br /> <br />Ig.;?, <br />-:, ~"; <br />f';<:i-":. <br />;:<.~ <br />,. <br />.~;<: <br />i~;' :,;:'; <br />;:~;::~::.: <br /> <br />