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<br />STATUS OF GREEN RIVER COLORADO PIKEMINNOW <br /> <br />1367 <br /> <br />0,18 <br />~ .16 <br />;::l ,14 <br />15.. <br />G ,12 <br />t: 0.1 <br />g ,08 <br />~ .06 <br />-g .04 <br />0: .02 <br />o <br /> <br /> <br />~ <br /> <br />o <br /> <br />200 <br /> <br />400 <br /> <br />600 <br /> <br />8013 1000 1200 <br /> <br />Colorado pikeminnow TL <br /> <br />FIGURE 5.-Probability of capture of Colorado pikeminnow <br />as a function of length for all 12 sampling passes (only years <br />are identified) conducted in the Yampa River, Colorado, <br />2000-2003, Dashed lines with solid squares represent passes <br />in 2000, solid lines passes in 2001, dashed lines passes in <br />2002 (the lowermost two passes overlap completely), and <br />solid lines with open circles passes in 2003. <br /> <br />onstrated a strong quadratic effect for fish size. The <br />logit parameter values are as follows: TLN = 0.2392 <br />(SE = 0.0845) and TLN2 = -0.1904 (0.0526); the <br />maximum transformed p's for the indlividual reaches, <br />years, and passes are given in Table 3. This result <br />stems from the fact that small and large fish had <br />relatively low capture probabilities and fish from about <br />500-600 mm TL had the highest ones (see Figure 5, in <br />which Yampa River fish are used as a representative <br />example of the variation observed). It should be noted <br />that the estimated probabilities of capture may be <br />functions of factors other than abundance (e.g., <br />behavior or habitat use) that make fish in a certain <br />size-class more or less prone to capture. <br />Probabilities of capture were relatively low and <br />varied widely (0.01-0.20) among sampling passes, <br />reaches, and years (Table 3). Average probabilities of <br />capture were slightly higher for the Vv'hite River and <br />the lower Green River than for other reaches. Average <br />annual values were lower for most river reaches in <br />2002 and 2003, which were drought years character- <br />ized by short runoff periods and low maximum <br />discharge levels. Average probabilities of capture <br />tended to remain the same or to increase from passes <br />1 to 3 in some reaches, even when fourth-pass data <br />were not combined with third-pass data. <br /> <br />Probabilities of Transition <br /> <br />The low frequency (mean much less than 1 %) of <br />transitions between sampling passes conducted in a <br />single year did not justify our sampling pass-specific <br />I/1's. Transition probabilities that characterized the <br />annual likelihood that tagged Colorado pikeminnow <br />would move among the five different Green River <br /> <br />TABLE 6.-Annual transition probabilities (I/t, i.e., proba- <br />bilities of movement to a different reach between years) for <br />average-size Colorado pikeminnow (500.4 mm TL) captured <br />in the Green River basin, 2000-2003. River reaches are as <br />follows: Yampa River (rlan 192 to rlan 74), White River (rlan <br />167.4 to rlan 0), middle Green River (rlan 539.4 to rkm <br />396,1), Desolation-Gray Canyon (Green River; rkm 395.9 to <br />rlan 206.1), and lower Green River (rlan 193.2 to rkm 0), <br /> <br />Reach shift 1\1 95% CI <br />White to Yampa 0.007 O,OOI-(J.055 <br />White to middle Green 0,048 0,022-0,102 <br />White to Desolation-Gray 0.080 0,043-0,144 <br />White to lower Green 0,003 0,000-0,067 <br />Yampa to White 0 <br />Yampa to middle Green 0.036 0,009-0,135 <br />Yampa 10 Desolation-Gray 0,018 0,003-0,122 <br />Yampa to lower Green 0 <br />Middle Green to White 0,022 O,Oll-O,045 <br />Middle Green to Yampa 0,018 0,007-0,045 <br />Middle Green to Desolation-Gray 0,045 0,024--0,081 <br />Middle Green to lower Green 0,001 O,OOO-O,1l5 <br />Desolation-Gray to White 0,032 0,010-0,099 <br />Desolation-Gray to Yampa 0 <br />Desolation-Gray to middle Green 0,078 0.031-0,186 <br />Desolation-Gray to lower Green 0,041 0,012-0.131 <br />Lower Green to White 0 <br />Lower Green to Yampa 0 <br />Lower Green to middle Green 0 <br />Lower Green to Desolation-Gray 0,121 0,048-0,274 <br /> <br />basin river reaches were low during the sampling <br />period, especially those for nonadjacent reaches (e.g., <br />the lower Green River to the White or Yampa River; <br />Table 6). Reaches in the middle of the study area had <br />the most fish moving in. For example, the Desolation- <br />Gray Canyon reach was the only reach to have fish <br />moving in from every other reach. The negative slope <br />for covariate TL reflected the fact that transition <br />probabilities among reaches were higher for smaller <br />fish (Figure 6). Transitions may reflect relatively short- <br /> <br />--<>- LG-DG - DG-LG <br />- -. 'DG-MG ~MG-YR <br /> <br />g 0.4 <br />:B <br />'" <br />..c 0,3 <br />0 <br /><:;., <br />'" 0,2 <br />.g <br />';;) <br />'" 0.1 <br />'" <br />~ - .. .. .. .. .. <br /> 0 <br /> 300 400 500 600 700 800 900 <br /> <br /> <br />Colorado pikeminnow TL <br /> <br />FIGURE 6,-Annual transition probabilities for Colorado <br />pikeminnow of different lengths for various reach combina- <br />tions in the Green River basin, 2000-2003. Abbreviations are <br />as follows: LG = the lower Green River reach, DG = the <br />Desolation-Gray Canyon reach, MG = the middle Green <br />River reach, and YR = the Yampa River. <br />