<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 />
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