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From: on behalf of Panel Registry Subject: FW: TNG registration of ...

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Taseko River drainages were extremely important and as such have invested a great deal <strong>of</strong> time<br />

and funding in the m<strong>on</strong>itoring and assessment <strong>of</strong> these runs. The following Table 9 shows sockeye<br />

and Chinook escapement data for the Chilko River. 60 The trend is further evidence that these stocks<br />

are<br />

in decline. It should be noted that the 2009 Chinook escapement is from the 2004 brood year<br />

that<br />

saw 16,287 adult Chinook return to spawn.<br />

Table 9: Salm<strong>on</strong> (Sockeye and Chinook) escapement to the Chilko River 1993­2009.<br />

Year Sockeye Chinook Year Sockeye Chinook<br />

1993 555226 6343 2001 668783 10891<br />

1994 450745 5665 2002 382814 11027<br />

1995 534559 10461 2003 608321 21625<br />

1996 974349 17000 2004 91909 16287<br />

1997 985827 16272 2005 535967 7668<br />

1998 879017 14549 2006 468947 5201<br />

1999 891922 8920 2007 305853 4366<br />

2000 758941 9171 2008 249863 5186<br />

2009 217572<br />

(preliminary)<br />

Source:<br />

Data provided by Fisheries and Oceans biologist Linda Stevens <strong>of</strong> Williams Lake.<br />

How climate change impacts fish<br />

8548<br />

(preliminary)<br />

While there are many negative influences <strong>on</strong> both anadromous and n<strong>on</strong>‐anadromous fish stocks,<br />

including over‐fishing, climate change is now c<strong>on</strong>sidered to be <strong>on</strong>e <strong>of</strong> the greatest threats to fish<br />

stocks throughout the world, including British Columbia and the Pacific Ocean. In its<br />

comprehensive<br />

Fourth Assessment Report in 2007, the Intergovernmental <strong>Panel</strong> <strong>on</strong> Climate Change<br />

( IPPC) states: “There is high c<strong>on</strong>fidence, based <strong>on</strong> substantial new evidence, that observed changes in<br />

marine and freshwater biological systems are associated with rising water temperatures, as<br />

well as related changes in ice cover, salinity, oxygen levels and circulati<strong>on</strong>. These include:<br />

shifts in ranges and changes in algal, plankt<strong>on</strong> and fish abundance in high­latitude<br />

oceans; increases in algal and zooplankt<strong>on</strong> abundance in high­latitude and highaltitude<br />

lakes; and range changes and earlier fish migrati<strong>on</strong>s in rivers [emphasis<br />

added]. While there is increasing evidence <strong>of</strong> climate change impacts <strong>on</strong> coral reefs,<br />

separating the impacts <strong>of</strong> climate­related stresses from other stresses (e.g. overfishing and<br />

polluti<strong>on</strong>) is difficult. {WGII 1.3, SPM}” (IPCC²).<br />

The <strong>Panel</strong>’s statement reflects the impact climate change will very likely have <strong>on</strong> both freshwater<br />

and marine aquatic envir<strong>on</strong>ments. Additi<strong>on</strong>ally, climate change is projected to not <strong>on</strong>ly affect<br />

anadromous species such as salm<strong>on</strong>, but also n<strong>on</strong> anadromous species, such as rainbow trout, Dolly<br />

Varden, Bull Trout, and Kokanee, all <strong>of</strong> which currently provide food for the Xeni Gwet’in<br />

community from lakes and streams<br />

in their Caretaker Area.<br />

60 Data provided by Fisheries and Oceans biologist Linda Stevens <strong>of</strong> Williams Lake.<br />

45

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