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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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including Shuswap <strong>and</strong> North Thompson. Some of the <strong>data</strong> go back 100 years, some just 10years. The Coldwater has two gauges, for example, so it’s on a pretty fine scale.Hinch: The <strong>Fraser</strong> <strong>River</strong> Environmental Watch program also has a large monitoring programindependent of that one. It generally operates from spring to fall, with <strong>data</strong> up the <strong>Fraser</strong>mainstem <strong>and</strong> in many of the tributaries since the mid/ late 1990s. Dave Patterson canprovide more information.Routledge: It seems almost like an impossible task. You get all this <strong>data</strong> <strong>and</strong> look for patterns butI suspect that if there are <strong>impacts</strong>, they will be local <strong>and</strong> subtle, such as warm water duringthe return migration on the Horsefly.Peterman: You won’t have ideal <strong>data</strong> sets for all CUs but you may have very useful <strong>data</strong> just forsome, so you should not rule it out if you don’t have <strong>data</strong> for all.Marmorek: We can look at stressor vs. productivity to see if there is a positive, negative orneutral correlation, for example if there is any difference in productivity in areas that havebeen most or least impacted by the Mountain Pine Beetle.Martin: Re <strong>cumulative</strong> effects <strong>and</strong> the graph that says the portfolio stays fairly constant overtime, one way of looking at that is that despite the variation in individual stocks, the <strong>Fraser</strong> isvery resilient because of those different stocks. That you have the same portfolio over 60years highlights the resilience.Pickard: The reality might be multiple stressors.Routledge: It’s upsetting to see the decline in the number of people who are actually out lookingat what’s happening in the Horsefly, for example. We’re sitting here looking at <strong>data</strong> setsinstead of talking to people who actually see things happening <strong>and</strong> that poses the risk ofmissing something.PICES advisory report on the decline of <strong>Fraser</strong> <strong>River</strong> Sockeye <strong>salmon</strong>in relation to marine ecologySkip McKinnell, PICESThe presentation opened with a quote from a 1909 media report describing the “discovery” by apre-eminent ichthyologist that the marine refuge for <strong>Fraser</strong> <strong>salmon</strong> between the time they leavethe river <strong>and</strong> the time they return to spawn is located 10 miles off Vancouver Isl<strong>and</strong>. Thefollowing slide showed <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> tagging locations spanning the entire NortheastPacific. This, McKinnell noted, highlights the difference between what we profess withoutadequate observations <strong>and</strong> what we know when there is relevant <strong>data</strong>.This project looked at marine factors that might be linked to the low <strong>sockeye</strong> returns in 2009 aswell as the gradual decline in productivity.It turns out that <strong>Fraser</strong> <strong>River</strong> <strong>sockeye</strong> smolts that went to sea in 2005 had the lowest survival onrecord (many scientists anticipated that). Those that went to sea in 2007 had the second lowestsurvival overall, except for Harrison <strong>sockeye</strong>, which had the highest total survival on record.The winter of 2006/2007 was an “official” El Nino. Each El Nino is different but severalcharacteristics are fairly common, including lower than average sea level pressure in the Gulf ofAlaska, an eastward shift in storm tracks <strong>and</strong> intensification of storms. Wind patterns tend tofollow the pressure contours, which in the winter of 2007 were blowing towards the BC central49

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