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which represent streams, inflows (natural runoff), reservoirs and diversions <br />that exist in the basin. The model simulates the amount of water flowing in <br />each link (stream reachy and the amount of water contained in each reservoir <br />while taking account of consumptive use by various water users. 7his is done <br />on a monthly basis for each year being modeled. The selection of the years <br />used in the modeling is discussed in the following section. <br />3.3 STUDY PERIOD HYDROLOGY <br />The first steps in developing the basin model were to select the <br />historical period to be studied and to compute virgin flows (flows wfiich would <br />have occurred without the effects of stream regulation or diversions) for that <br />study period. The study period consisted of 384 consecutive months from <br />October 1952 through September 1983. This period was selected because it is <br />statistically similar to the total period of record for three key streamflow <br />gaging stations in the basin and includes a variety of hydrologic conditions. <br />Nearly all the significant dry years in the period of record were included in <br />the selected study period. <br />Separate data files of monthly virgin flows were derived for 59 locations <br />in the basin. Virgin flows at gaged sites were derived frc��� historical flow <br />records corrected for upstream reservoir operations, basin imports and <br />exports, and irrigation depletions. Historical irrigation depletions were <br />estimated from climatic data, consumptive use calculations, diversion records, <br />and detailed operating studies of selected ditches. Uirgin flows at ungaged <br />sites were developed from virgin flows at gaged sites corrected for area and <br />elevation differences. <br />3.4 REPRESENTATION OF WATER RIGHTS <br />Gunnison basin water rights are represented in the model in one of two <br />ways. "Select" water rights which significantly influence river <br />administration or which transfer water from one sub-basin to another are <br />3-2 <br />