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Last modified
7/14/2009 5:02:37 PM
Creation date
5/20/2009 1:34:57 PM
Metadata
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UCREFRP
UCREFRP Catalog Number
9665
Author
Schmidt, J. C. and J. B. Box.
Title
Controls on the Longitudinal Distribution of Age-0 Colorado Pikeminnow in the Middle Green River, Colorado and Utah - Draft Report.
USFW Year
2001.
USFW - Doc Type
Logan, UT.
Copyright Material
NO
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<br /> <br />fr..~ <br />L, ,)J <br /> <br />295265 in 1991, reach 265250 in 1991 anA'992, an~ reach 240230 in 1991. ~us, CPE was <br />larger in 1991 than in 1990, despite the fact that the drift was twice as large in 1990 and the <br />~ hydrology was nearly the same') <br />).. ~ . Reaches are designated by distance of the reach boundaries upstream from the confluence <br />~ __ \ of the Green and Colorado Rivers. These locations are in river miles, because this river location <br />to ~ I system h~ long.been in use in the region. Thus, reach 310300 is 16.7 kIn long and is located <br />. J . i hetw_een nver mIles 310 and 300. <br />'4 \ ~ Other sampling provides conllicting perspectives on the relative size of larval populations <br />. between 1990 and 1991. JuvenIle plkemmnow samplIng mdlcate that recrUitment from the 1990 <br />larval population was greater than from the 1991 population, because 41 juvenile fish were collected <br />in fall 1991 and none in fall 1992 (McCada, unpubl. data). However, Valdez and Cowdell (1999) <br />sampled 281 age-O pikeminnow in fall 1990 and 526 in fall 1991 in reach 265250, indicating larger <br />arval populations in 1991. >f ,.~ "} <br />The standard error of the mean CPE is typically large, because of the large variability in the <br />number of pikeminnows collected in each sampled backwater, the high proportion of seine hauls <br />with no fish, and the few number of backwaters sampled. Differences in the mean CPE of each <br />reach beyond the standard error only occurred in 1992 and 1993, when reach 265250 had higher <br />CPE than elsewhere. In other years, the reach standard errors were too large to identify distinctive <br />characteristics in the longitudinal distribution of larval pikeminnows. In these circumstances where <br />a small proportion of the population is sampled, a simulation model offers an attractive alternative in <br />the evaluation of population distributions and the factors that control that distribution. <br />Simulation Model of Drift and Transport into Backwaters <br /> <br />11/14/01 draft report, Schmidt and Box <br /> <br /> <br />""J <br />.. <br />/ <br /> <br />Overview <br />We developed a simulation model of larval drift and transport into backwaters in order to <br />predict the distribution of age-O fish. The simulation model integrates hydrologic, geomorphic, and <br />biologic factors and was written using Stella Research Software (High Performance Systems, <br />1996). The model is structured such that a cohort of larval fish enters the Green River each day <br />from the Yampa River, and these fish drift downstream through 10 reaches that are between 8 and <br /> <br />,~ <br />~" 50 kIn long (Appendix A). Reaches were defined on the basis of geomorphic characteristics of the <br />~ ,r"\ channel, alluvial valley, and the location of tributaries. Since the YampaRiveris the only source of <br />. f ,r\) larval fish into the study area, we compared field measurements with model predictions. <br />J ;J' L j~. The predicted time it takes larvae to drift through each reach is determined by reach length, <br />) r:! I- flow velocity, and whether larvae remain in the main cunen! or are transported into backwaters. We <br />assumed that larvae drift at the mean velocity of the stream. We recognize that this assumption may <br />"f/ . \:" over-predict the rate of movement of larvae through reaches, but more accurate predictions of the <br />V.i<~te of drift necessitate field studies. . <br /> <br />'r <br /> <br />" l:J' <br />o ~ <br />y\j >r <br />IIll... <br /> <br />8 <br />
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