Anticipating the consequences of climate change for Canada’s boreal forest ecosystems

Author:

Price David T.1,Alfaro R.I.2,Brown K.J.2,Flannigan M.D.1,Fleming R.A.3,Hogg E.H.1,Girardin M.P.4,Lakusta T.5,Johnston M.6,McKenney D.W.3,Pedlar J.H.3,Stratton T.7,Sturrock R.N.2,Thompson I.D.3,Trofymow J.A.2,Venier L.A.3

Affiliation:

1. Canadian Forest Service, Natural Resources Canada, Northern Forestry Centre, 5320 122 Street, Edmonton, AB T6H 3S5, Canada.

2. Canadian Forest Service, Natural Resources Canada, Pacific Forestry Centre, 506 West Burnside Road, Victoria, BC V8Z 1M5, Canada.

3. Canadian Forest Service, Natural Resources Canada, Great Lakes Forestry Centre, 1219 Queen Street East, Sault Ste. Marie, ON P6A 2E5, Canada.

4. Canadian Forest Service, Natural Resources Canada, Laurentian Forestry Centre, 1055 du P.E.P.S., P.O. Box 10380, Stn. Sainte-Foy, QC G1V 4C7, Canada.

5. Forest Management, Environment and Natural Resources, Government of the Northwest Terrritories, Station Main, Yellowknife, NT X1A 2L9, Canada.

6. Saskatchewan Research Council, 15 Innovation Blvd., Saskatoon, SK S7N 2X8, Canada.

7. Alberta Environment and Sustainable Resource Development, 12th Floor, Baker Centre, 10025 106 Street, Edmonton, AB T5J 1G4, Canada.

Abstract

Canadian boreal woodlands and forests cover approximately 3.09 × 106 km2, located within a larger boreal zone characterized by cool summers and long cold winters. Warming since the 1850s, increases in annual mean temperature of at least 2 °C between 2000 and 2050 are highly probable. Annual mean temperatures across the Canadian boreal zone could be 4–5 °C warmer than today’s by 2100. All aspects of boreal forest ecosystem function are likely to be affected. Further, several potential “tipping elements” — where exposure to increasing changes in climate may trigger distinct shifts in ecosystem state — can be identified across the Canadian boreal zone. Approximately 40% of the forested area is underlain by permafrost, some of which is already degrading irreversibly, triggering a process of forest decline and re-establishment lasting several decades, while also releasing significant quantities of greenhouse gases that will amplify the future global warming trend. Warmer temperatures coupled with significant changes in the distribution and timing of annual precipitation are likely to cause serious tree-killing droughts in the west; east of the Great Lakes, however, where precipitation is generally nonlimiting, warming coupled with increasing atmospheric carbon dioxide may stimulate higher forest productivity. Large wildfires, which can cause serious economic losses, are expected to become more frequent, but increases in mean annual area burned will be relatively gradual. The most immediate threats could come from endemic forest insect pests that have the potential for population outbreaks in response to relatively small temperature increases. Quantifying the multiple effects of climate change will be challenging, particularly because there are great uncertainties attached to possible interactions among them, as well as with other land-use pressures. Considerable ingenuity will be needed from forest managers and scientists to address the formidable challenges posed by climate change to boreal ecosystems and develop effective strategies to adapt sustainable forest management practices to the impending changes.

Publisher

Canadian Science Publishing

Subject

General Environmental Science

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