Juvenile Life History of Wild Fall Chinook Salmon in the Snake and Clearwater Rivers
By W. Connor, H. L. Burge, R. Waitt, T. C. Bjornn. 2002
92 citations recorded by the source corpus.
Subfields: Ecology, Nature and Landscape Conservation, Water Science and Technology
View Paper: https://www.semanticscholar.org/paper/a0345ce42845ed4b5f971d68144596acd8a703a0
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In Ecology
In Nature and Landscape Conservation
Citations in the corpus
- Two Alternative Juvenile Life History Types for Fall Chinook Salmon in the Snake River Basin (2005, background): “The Snake River from the Salmon River confluence to Hells Canyon Dam (hereafter, Snake River upper reach; Figure 1 ) is the warmest spawning area, and it offers a relatively high level of opportunity for growth. For example, in 1995, mean temperature during rearing averaged 12°C; young fall Chinook”
- 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): “Not only fry emergence, as discussed above, but also growth to parr size and smolt emigration (Connor et al., 2002), indicate the strong effect of water temperature.”
- Influence of Flow and Temperature on Survival of Wild Subyearling Fall Chinook Salmon in the Snake River (2003, unknown): “during summer in contrast to their pre-dam counterparts that migrated seaward in late spring (Connor et al. 2002).”