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Fraser River sockeye salmon: data synthesis and cumulative impacts

Fraser River sockeye salmon: data synthesis and cumulative impacts

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2011). The thermal limit hypothesis describes the role that ocean temperature has in limiting thegeographic range of <strong>sockeye</strong> <strong>salmon</strong> in the North Pacific, <strong>and</strong> suggests how this range may bereduced by warming ocean temperatures due to climate change. But McKinnell et al. (2011,Section 3.5) critique this theory because it does not consider the ability of <strong>sockeye</strong> <strong>salmon</strong> toseek cooler ocean temperatures simply by moving deeper. Inter-annual <strong>and</strong> inter-decadalvariation in ocean temperature <strong>and</strong> biological productivity are known to have substantial <strong>impacts</strong>on many marine species (McKinnell et al., 2011).Such variability in ocean conditions may be further exacerbated by climate change. Forexample, in recent decades the Pacific Decadal Oscillation has been exhibiting more frequentoscillations between phases (Hinch <strong>and</strong> Martins, 2011, Section 1.5). Hinch <strong>and</strong> Martins (2011)suggest that “it seems that interannual variations in climate conditions have contributed to theextreme variation in the abundance of returning adults that were observed in 2009 <strong>and</strong> 2010”.Habitat conditions in the Strait of Georgia, including marine conditions <strong>and</strong> human activities<strong>and</strong> development are obviously not factors during the open ocean phase, but the samemechanisms described in Section 4.4 are relevant for returning adults. Returning adults maypotentially be more resilient to some of the stressors encountered through the Strait of Georgia,especially since returning individuals are those that have survived the early marine phase <strong>and</strong>two winters in the open ocean.4.5.2 Exposure of <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> to stressorsThe ability to assess the exposure of <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> <strong>salmon</strong> to various potential stressorsin the open ocean <strong>and</strong> return journey to B.C. coastal waters is severely limited by lack ofknowledge of the distribution of <strong>sockeye</strong> <strong>salmon</strong> during this stage. McKinnell et al. (2011,Section 1.3) describe the lack of systematic monitoring <strong>and</strong> report that “there are virtually noobservations of <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> <strong>salmon</strong> during about 75% of their life at sea <strong>and</strong> the valueof coincidental samples taken during their emigration from the Strait of Georgia is debatable”.Aside from the following case where there is some information with which to evaluate exposure,one must simply assume that the <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> <strong>salmon</strong> have been exposed to themechanisms described above.The evidence presented by Christensen <strong>and</strong> Trites (2011) shows that for marine mammalpredators there has not been exposure to California sea lions because they are not present alongthe southern coast of BC during the summer. However, Steller sea lions have a large populationdistributed along with the northern <strong>and</strong> western coasts of Vancouver Isl<strong>and</strong> during the summer<strong>and</strong> the total population for BC <strong>and</strong> southeast Alaska may be upwards of 60,000 (Peterman et al.73

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