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Last modified
7/14/2009 5:02:33 PM
Creation date
5/22/2009 5:29:52 PM
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UCREFRP
UCREFRP Catalog Number
8178
Author
Anderson, R. and G. Stewart.
Title
Riverine Fish Flow Investigations.
USFW Year
1999.
USFW - Doc Type
Fort Collins, CO.
Copyright Material
NO
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />State: Colorado <br /> <br />Project No. 7400 ENDG 0700 <br /> <br />Name: Aquatic Nongame Research <br /> <br />Study No. SE-3-22 <br /> <br />Title: Riverine Fish Flow Investigations <br /> <br />Period Covered: July 1. 1997 - June 30.2002 <br /> <br />Study Objective: <br /> <br />To determine relationships between flow and habitat availability <br />for warm-water riverine fish communities of Colorado. <br /> <br />INTRODUCTION <br /> <br />Habitat loss is one of the single greatest causes of decline in populations of <br />native fishes in North America (Williams et al. 1989). While there clearly must be some <br />minimum flow needed to maintain a healthy, functioning river community, methods to <br />establish minimum flows on warm water river sections have proved controversial. Most <br />in stream flow studies implemented in Colorado have focused on protecting minimum <br />stream flow for cold water (headwater) habitats using either the R2Cross method <br />(Nehring 1979) or Instream Flow Incremental Methodology (IFIM) (Bovee 1982), <br />which determines habitat availability based on a single target species. IFIM estimates <br />the amount of usable habitat for fish as a function of discharge by combining habitat <br />suitability curves with the hydraulic model. The habitat component of the model has <br />received much criticism because of assumptions implicit with using suitability curves <br />and assumptions of positive relationships between habitat availability and fish <br />abundance. Validation of these assumptions have been obstacles for successfully using <br />IFIM to model minimum flow impacts on large warm water rivers of the west slope <br />(Rose and Hahn 1989). <br /> <br />Warm water fish assemblages appear to require a more intensive approach to <br />in stream flow modeling compared to cold water fish communities. Warm water river <br />reaches tend to be lower gradient and have higher channel complexity and.sediment <br />loads. Warm water fish populations tend to have higher species diversity. Also habitat <br />suitability curves derived from microhabitat observations do not adequately describe <br />habitat use for many warm water species. A broad community-level perspective, as <br />opposed to an indicator species approach, may be required to protect all habitats of a <br />functioning warm water stream ecosystem. <br /> <br />Instream flow techniques require integration of two processes that combine <br />detailed knowledge of habitat requirements (by species and life stage), and the <br />availability of necessary habitats. Both the collection and analysis of these data bases <br />have been very labor intensive. Recent advances in surveying techniques (e.g. G.P.S.) <br />and computer capabilities (G.I.S.) allow for collection and processing of much larger <br />databases. Also, two-dimensional (2-D) flow models may have potential for application <br />in in stream flow studies (Leclerc et al., 1995; Bovee, 1996). In theory, 2-D models offer <br />a significant improvement over one-dimensional (I-D) modeling by increasing spatial <br /> <br />1 <br />
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