Migration Timing, Growth, and Estimated Parr‐to‐Smolt Survival Rates of Wild Snake River Spring–Summer Chinook Salmon from the Salmon River Basin, Idaho, to the Lower Snake River

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A review of the likely effects of climate change on anadromous Atlantic salmon Salmo salar and brown trout Salmo trutta, with particular reference to water temperature and flow. (2009, background): “found in some Idaho and Oregon rivers (Roper & Scarnecchia, 1999; Achord et al., 2007).”
Synchronization and portfolio performance of threatened salmon (2010, background): “Pacific salmon exhibit fine-scale population structure and local adaptations to their natal habitats (e.g., Achord et al. 2007), which likely contributes to asynchrony in population dynamics (Hilborn et al. 2003; Rogers & Schindler 2008; Greene et al. 2009).”
Temperature and Flow Effects on Migration Timing of Chinook Salmon Smolts (2009, background): “Downstream movement of parr in the summer and fall has been documented in a number of streamtype populations (upper Fraser River: Bradford and Taylor 1997; Snake River: Bjornn 1971; Achord et al. 2007).”
Nonlethal Sampling of Fish Caudal Fins Yields Valuable Stable Isotope Data for Threatened and Endangered Fishes (2009, methodology): “Juvenile Chinook salmon and steelhead were collected from 21 tributaries using electrofishing and seining techniques from late July through September from 2003 to 2005 ( Figure 1 ). Study sites coincided with streams where juvenile salmonid survival has been monitored for over a decade ( Achord et a”