2015
DOI: 10.1002/rra.2934
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Assessing Juvenile Salmon Rearing Habitat and Associated Predation Risk in a Lower Snake River Reservoir

Abstract: Subyearling fall Chinook salmon (Oncorhynchus tshawytscha) in the Columbia River basin exhibit a transient rearing strategy and depend on connected shoreline habitats during freshwater rearing. Impoundment has greatly reduced the amount of shallow‐water rearing habitat that is exacerbated by the steep topography of reservoirs. Periodic dredging creates opportunities to strategically place spoils to increase the amount of shallow‐water habitat for subyearlings while at the same time reducing the amount of unsui… Show more

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Cited by 14 publications
(29 citation statements)
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“…The preference of juvenile Chinook Salmon for this type of habitat (Tiffan et al. ) may have provided Smallmouth Bass with better foraging opportunities that contributed to the often‐higher consumption rates in natural habitat.…”
Section: Discussionmentioning
confidence: 99%
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“…The preference of juvenile Chinook Salmon for this type of habitat (Tiffan et al. ) may have provided Smallmouth Bass with better foraging opportunities that contributed to the often‐higher consumption rates in natural habitat.…”
Section: Discussionmentioning
confidence: 99%
“…These are important rearing areas for subyearlings (Tiffan et al. ) and for active migrants that delay or slow their downstream movements through these habitats (Tiffan et al. ).…”
Section: Discussionmentioning
confidence: 99%
“…Mean water column velocity (cm s -1 ) was also included as a covariate in the Lower Granite Reservoir model because velocity data were available for that reservoir. Velocities were estimated for each trawl transect from a two-dimensional hydrodynamic model (Tiffan et al 2015) as follows. First, at each transect, velocities were estimated at each of the five discharges (1388,3342,4050,4361, and 5664 m 3 s -1 ) modeled by Tiffan et al (2015).…”
Section: Spatiotemporal Distributionmentioning
confidence: 99%
“…Velocities were estimated for each trawl transect from a two-dimensional hydrodynamic model (Tiffan et al 2015) as follows. First, at each transect, velocities were estimated at each of the five discharges (1388,3342,4050,4361, and 5664 m 3 s -1 ) modeled by Tiffan et al (2015). These were then used to construct 96 transect-specific regressions to predict velocity from discharge (mean r 2 = 0.97, range 0.07-0.99).…”
Section: Spatiotemporal Distributionmentioning
confidence: 99%
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