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Table 2. Step -trend results on the daily mean streamflow at station 07096000 (Arkansas River at Canon City) between <br />1964 -74 and 1975 -94 <br />[ft3 /s, cubic feet per second; N, number of values; p value is the significance level of the test; <, less than; NS, trend not statistically significant; <br />I, statistically significant increasing trend; D, statistically significant decreasing trend] <br />to statistically significant trend was defined as having a p value less than or equal to 0.05. <br />180,000 <br />W <br />LL 160,000 <br />W <br />rY <br />U <br />Q <br />Z 140,000 <br />W <br />F- <br />Q <br />120,000 <br />W <br />Cr <br />O <br />0- 100,000 <br />LL <br />O <br />W <br />80,000 <br />J <br />0 <br />J <br />n 60,000 <br />Z <br />Z <br />Q <br />J <br />Q <br />O 40,000 <br />F- <br />20,001963 1965 <br />1970 1975 1980 1985 1990 1995 <br />Figure 6. Total annual volume of water imported into the Arkansas River from the Colorado River Basin, 1964 -94. <br />14 Relations of Streamflow and Specific- Conductance Trends to Reservoir Operations in the Lower Arkansas <br />River, Southeastern Colorado <br />1964 -74 <br />1975 -94 <br />Month <br />Median <br />Median <br />p value <br />Significancel <br />streamflow <br />N <br />streamflow <br />N <br />(ft3/S) <br />(n3/S) <br />January <br />304 <br />341 <br />378 <br />620 <br /><0.01 <br />I <br />February <br />284 <br />308 <br />351 <br />560 <br /><01 <br />I <br />March <br />268 <br />341 <br />385 <br />620 <br /><0I <br />I <br />April <br />268 <br />330 <br />369 <br />600 <br /><.01 <br />I <br />May <br />874 <br />341 <br />792 <br />620 <br />.16 <br />NS <br />June <br />1,800 <br />330 <br />2,140 <br />600 <br />.04 <br />I <br />July <br />1,420 <br />341 <br />1,150 <br />620 <br /><01 <br />D <br />August <br />1,020 <br />341 <br />703 <br />620 <br /><.01 <br />D <br />September <br />380 <br />330 <br />369 <br />600 <br />.04 <br />D <br />October <br />232 <br />341 <br />329 <br />620 <br /><01 <br />I <br />November <br />344 <br />330 <br />425 <br />600 <br /><.01 <br />I <br />December <br />344 <br />341 <br />412 <br />620 <br /><.01 <br />I <br />to statistically significant trend was defined as having a p value less than or equal to 0.05. <br />180,000 <br />W <br />LL 160,000 <br />W <br />rY <br />U <br />Q <br />Z 140,000 <br />W <br />F- <br />Q <br />120,000 <br />W <br />Cr <br />O <br />0- 100,000 <br />LL <br />O <br />W <br />80,000 <br />J <br />0 <br />J <br />n 60,000 <br />Z <br />Z <br />Q <br />J <br />Q <br />O 40,000 <br />F- <br />20,001963 1965 <br />1970 1975 1980 1985 1990 1995 <br />Figure 6. Total annual volume of water imported into the Arkansas River from the Colorado River Basin, 1964 -94. <br />14 Relations of Streamflow and Specific- Conductance Trends to Reservoir Operations in the Lower Arkansas <br />River, Southeastern Colorado <br />