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<br />, <br /> <br />;~(i~;f' <br /> <br />~~~}i <br /> <br />n0~'7R7 <br />'-.I '_1 J . '.J J <br /> <br />attributable to gagirg accuracy) from the Gunnison River at Crystal Dam. The <br /> <br />occurrence of negative values above an assumed allowable gagirg error may be <br />.~~ <br /> <br />attributed to assumptions made in accountirg for reservoir effects in virgin <br /> <br />flow development at the Gunnison River at Crystal Dam base station. <br /> <br />Bank storage effects are computed as a constant percentage of Blue Mesa <br /> <br />Reservoir monthly charge in content (10 percent). Actual bank storage'and <br /> <br />release, both pattern and quantity, may be different. <br /> <br />Reservoir evaporation is accounted for usirg fixed monthly evaporation <br /> <br />rates multiplied by reservoir area. No consideration was made for fluctuation <br /> <br />in monthly evaporation rates on a year-to-year basis. <br /> <br />In addition, reservoir effects (i.e., bank storage and evaporation) are <br /> <br />not taken into account for all reservoirs. <br /> <br />The second difference file was developed for the virgin flow core . f." <br /> <br />. <br /> <br />stations above the Gunnison River near Gunnison (09114500): Ohio Creek near <br /> <br />Gunnison (09114000), East River at Almont (09112500), and Taylor River at <br /> <br />Almont (09110000) virgin flow core stations (see Figure 1). Core station <br /> <br />files used to derive this difference file are shown in Table 4. <br /> <br />8 <br />