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A second, system-wide trend revealed by these data is the distinct period from the late 1950s <br />through the late 1970s when annual sediment loads were much lower than the period before or <br />after. Pitlick et al. (1999) have previously suggested that significant amounts of sediment would <br />have been deposited in the channel during this time, which may have had long-lasting effects on <br />native fish populations. The statistical significance of these differences was evaluated here using <br />the Mann-Whitney test, a nonparametric procedure that is appropriate for situations in which the <br />assumptions of standard parametric procedures are not satisfied (e.g. if the data are not normally <br />distributed). The Mann-Whitney test is essentially a test of differences in means (similar to the t- <br />test), but rather than comparing the data themselves, the test examines differences in the ranks of <br />individual values (Berenson et al., 1988). Two samples are considered to be statistically different if <br />they contain disproportionate numbers of highly or lowly ranked values. Comparisons were made <br />between two periods, 1934-58 and 1959-97; the State Line gauge was excluded from the analysis <br />because the record includes only five years prior to 1958. <br />a) Colorado River at Glenwood Springs <br />a <br />1.5 <br />c <br />m <br />1.0 <br />c <br />m <br />CL <br />0.5 <br />w <br />150 <br />E 0.0 <br />m <br />? 100 <br />m <br />r <br />a 50 <br />a <br />c <br />c p <br />1930 1940 1950 1960 1970 1980 1990 2000 <br />b) Colorado River near Cameo <br />A <br />3 <br />4.0 m <br />3.0 <br />0 <br />m <br />CL <br />2.0 <br />a <br />A 30G 10 <br />5 <br />m 0.0 <br />200 <br />L <br />V <br />0 100 <br />W <br />7 <br />C <br />C Q <br />a <br />1930 1940 1950 1960 1970 1980 1990 2000 <br />Figure 14. Trends in annual discharge and suspended sediment load at (a) Glenwood Springs and <br />(b) Cameo. Horizontal lines indicate means for the periods 1934-1958 and 1959-1997. <br />24