Environmental Change in the Great Whale River Region, Hudson Bay: Five Decades of Multidisciplinary Research by Centre D’Études Nordiques (CEN)1
18 (3): 182-203 (2011) Environmental change in the Great Whale River region, Hudson Bay: Five decades of multidisciplinary research by Centre d’études nordiques (CEN)1 Najat BHIRY2, Centre d’études nordiques and Département de géographie, Université Laval, Québec, Québec, Canada. Ann DELWAIDE, Centre d’études nordiques, Université Laval, Québec, Québec, Canada. Michel ALLARD, Centre d’études nordiques and Département de géographie, Université Laval, Québec, Québec, Canada. Yves BÉGIN, Centre d’études nordiques and INRS - Centre Eau Terre Environnement, Québec, Québec, Canada. Louise FILION & Martin LAVOIE, Centre d’études nordiques and Département de géographie, Université Laval, Québec, Québec, Canada. Christian NOZAIS, Centre d’études nordiques and Département de biologie, chimie et géographie, Université du Québec à Rimouski, Rimouski, Québec, Canada. Serge PAYETTE, Centre d’études nordiques and Département de biologie, Université Laval, Québec, Québec, Canada. Reinhard PIENITZ, Centre d’études nordiques and Département de géographie, Université Laval, Québec, Québec, Canada. Émilie SAULNIER-TALBOT, Centre d’études nordiques, Université Laval, Québec, Québec, Canada. Warwick F. VINCENT, Centre d’études nordiques and Département de biologie, Université Laval, Québec, Québec, Canada. Abstract: The Great Whale River region on the eastern shore of Hudson Bay, Canada, encompasses the villages of Whapmagoostui (Cree First Nation) and Kuujjuarapik (Inuit) and surrounding areas. The principal field station of Centre d’études nordiques (CEN: Centre for Northern Studies) has operated at Whapmagoostui-Kuujjuarapik (W-K; 55° 15' N, 77° 45' W) since the 1970s, with diverse research projects on past and present environments. The climate at W-K is strongly influenced by the proximity of Hudson Bay, and the recent pronounced loss of sea ice in this sector of northern Canada has been accompanied by large increases in air temperature.
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