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Last modified
7/14/2009 5:02:34 PM
Creation date
5/20/2009 3:39:59 PM
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UCREFRP
UCREFRP Catalog Number
8251
Author
Rakowski, C. L. and J. C. Schmidt.
Title
The Geomorphic Basis of Colorado Squawfish Nursery Habitat in the Green River Near Ouray, Utah.
USFW Year
1996.
USFW - Doc Type
#93-1070,
Copyright Material
NO
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<br />Draft Fmal Completion Report to UDWR for Contract #93-lOiO. Amendment 3 <br /> <br />v <br /> <br />redistribution of sediment and the large-scale response of the channel features to flood passage. <br /> <br />Three geomorphic settings create the majority of nursery habitat lli the 10-km study reach. These settings are <br /> <br />(1) the downstream end of secondary channels. (2) the upstream end of secondary channels. and (3) inactive chute <br /> <br />channels. The first and third of these settings are also the most common location of deep nursery habitats. Overall. a <br /> <br />small number of sites provide the majority of the total area of deep habitats in any year. <br /> <br />The number and size of these habitats changed from year to year in this study. The hig!1 magnitude flood of <br /> <br />1993 did not significantly increase the number or total area of deep nursery habitats. but the total number and area of all <br /> <br />habitats greatly decreased. In contrast, the number and area of deep habitats and total habitats decreased after passage of <br /> <br />the relatively small flood of 1994. The 1994 flood created more habitats than did the 1992 flood. <br /> <br />Analysis of the geomorphic settings of nursery habitats at the detailed study site show that different settings <br /> <br />create available habitat at different discharges (Fig. ES 1). Thus, the shape of discharge-dependent habitat availability <br /> <br />curves (HAC's) in any year is determined by the topographic relief and relative size of the geomorphic features that <br /> <br /> WATER SURFACE ElEV AllON. IN METERS <br /> 93.5 94.0 94.5 95.0 9 .5 <br /> 14000 <br />en <br />;12~ X <br />SECONDARY <br />CHANNEL ~~\ <br />~1(XX)Q <br />:J ISOLAlED <br />0 <br />en 8000 POOL <br />~ <br />~ V BAR rop <br />-< 6000 <br />~ <br />~ 4000 <br />>- I~\ ~-.. <br />Ii] <br />en 2000 I II ,..~, <br />~ I I I />1' <br />z <br /> 0 <br /> 0 50 100 ISO 200 250 300 3SO <br /> DISCHARGE. IN CUBIC METERS PER SECOND <br /> <br /> <br /> <br />FIGURE ES 1. Decomposition of the localized habitat availability curve by geomorphic classification. Area of <br />available habitat is separated into geomorphic components (for example, the habitats associated with the secondary <br />channel, superimposed bars. and isolated pools). Dashed and solid lines indicate 1993 and 1994 habitats, respectively. <br />. The total available habitat in 1993 and 1994 are indicated by X's and +'s, respectively. The lines do not always <br />coincide with the markers but the addition of the curves for available habitat in each geomorphic setting for each year <br />results in habitat availability curve shown in Figure 31. <br />
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