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Analysis of Historical Discharge Records 9 <br />5,000 <br />3,000 <br />U 2,000 <br />mo <br />~z <br />Z ~ 1,000 <br />ui ~ 700 <br />C7 <br />a a 500 <br />x~ <br />Uw <br />~ ~ 300 <br />0 <br />200 <br />100 <br />0.1 <br />0.0 <br />~ -0.1 <br />w <br />w <br />w <br />z -0.2 <br />F <br />w <br />2 <br />~ -0.3 <br />-0.4 <br />-0.5 <br />2 <br />w <br />U <br />Z <br />W <br />W 0 <br />LL <br />LL <br />D <br />W <br />C7 <br />Q <br />F <br />w -2 <br />U <br />w <br />a <br />-4 <br />• <br />• <br />I i I I <br />1995 1996 1997 1998 1999 2000 2001 2002 <br />WATER YEAR <br />Figure 4. Discharge, shift, and percentage difference between discharge and discharge rating for measurements <br />made at the below-Redlands-dam station, water years 1995-2002. <br />for the Whitewater and Redlands-Canal stations. For WYs water year (table 2). Excluding the partial data for WY 1995, <br />1995-2002, daily mean discharge was estimated for 85 days the differences between the annual sums of daily mean dis- <br />(out of 2,771) for the below-Redlands-dam station. charge at the two downstream stations and the annual sums of <br />Daily mean discharges at the two downstream stations daily mean discharges at the upstream station ranged from <br />(below-Redlands-dam and Redlands-Canal) were summed to about -28,700 to -69,800 acre-ft. The difference, as a percent- <br />produce an estimate of the downstream streamflow; this sum age of the upstream discharge, ranged from about -1.1 to <br />was subtracted from the daily mean discharge at the Whitewater -5.8 percent (table 2). These results indicate that the down- <br />station (the upstream streamflow). This difference provides an stream discharges generally were less than the upstream <br />estimate of the difference between downstream and upstream discharges. <br />streamflow along the study reach. These data were compiled for Moving 3-day daily mean discharges also were computed <br />each day of WYs 1995-2002, and the values were summed by for each of the three stations and the differences between the <br />