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<br />. <br /> <br />e <br /> <br />e <br /> <br />90112B <br /> <br />attributable to gaging accuracy) from the Gunnison River at Crystal Dam, The <br /> <br />occurrence of negative values above an assumed allowable gaging error may be <br /> <br />attributed to assumptions made in accounting 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 change 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 using 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 <br /> <br />stations above the Gunnison River near Gunnison (09114500), Ohio Creek near <br /> <br />Gunnison (09114000), East River at A1mont (09112500), and Taylor River at <br />Almont (09110000) virgin flow core stations (see F~ure 1), Core station <br />files used to derive this difference file are shown in Table 4, <br /> <br />8 <br />