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Fraser River sockeye salmon: data synthesis and cumulative impacts

Fraser River sockeye salmon: data synthesis and cumulative impacts

Fraser River sockeye salmon: data synthesis and cumulative impacts

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for all CUs should not rule out using existing <strong>data</strong>, but with caveats, <strong>and</strong> 3) caution that <strong>impacts</strong>may be local <strong>and</strong> subtle.PICES Advisory Report on the Decline of <strong>Fraser</strong> <strong>River</strong> SockeyeSalmon in Relation to Marine EcologySkip McKinnell, PICESThe main objective is to assemble a comprehensive summary of what is known about <strong>Fraser</strong><strong>River</strong> <strong>sockeye</strong> <strong>salmon</strong> in the ocean. Much of the study involved reviewing <strong>data</strong>/ technical reports<strong>and</strong> peer-reviewed literature, although some original <strong>data</strong> were re-analyzed. To explain the longtermdecline in <strong>sockeye</strong> <strong>salmon</strong>, McKinnel presented evidence that there was an abrupt “shift” tolower productivity in 1992 rather than a “trend” of a gradual decline in productivity. The lowreturns of 2009 are associated with the 2007 (2nd lowest) ocean entry year (OEY) for <strong>sockeye</strong><strong>salmon</strong>. The 2006/7 el Niño created extremes in discharges (runoff) on the central coast of BCthat may have affected the <strong>salmon</strong> by altering surface salinity. Furthermore, there were unusuallystrong southeasterly winds in the summer of 2007 (the most extreme since 1948), which keptfreshwater entrained in Queen Charlotte Sound (QCS). This raised the sea level <strong>and</strong> maintained alow salinity, freshwater “lens” in QCS, all of which delayed the spring bloom of algae (the latestsince records began to be collected in 1998). Additional evidence for ocean forcing were warmsurface sea temperatures (SSTs) in QCS in 2007.Data which extend the PSC report include: 1) the 2006 Harrison <strong>River</strong> brood year returns, 2)2004 Chilko Lake <strong>sockeye</strong> marine survival, <strong>and</strong> 3) 2007 weather, climate, oceanography <strong>and</strong>phenology of Queen Charlotte Sound/Strait. The most important unknowns for <strong>sockeye</strong> <strong>salmon</strong>in the ocean are the numbers of smolts entering the sea, by stock. There have been no studiesdocumenting where <strong>and</strong> when <strong>sockeye</strong> <strong>salmon</strong> die in the ocean.This presentation stimulated many questions from workshop participants including:o What’s the relative likelihood of different mechanisms that are not mutually exclusive?o Chums did poorly in 2010 <strong>and</strong> <strong>sockeye</strong> well, but both entered ocean in 2007 - why?o Why were conditions more extreme in QCS during 2007 than in Georgia Strait?o Could there have been harmful algae blooms in QCS as suggested in the PSC report?o Why didn’t Mackas or Peterson indices predict the low 2009 return?o Did you compare median recruits per spawner against Mackas red <strong>and</strong> blue years?o PSC report suggested that zooplankton production in 2007 was not anomalouso Can one really determine whether it’s a gradual or step change in productivity?o Can you explain other stock patterns (e.g., West Coast Vancouver Isl<strong>and</strong>, <strong>Fraser</strong> pinks)?

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