Table 2.3
Forest area and long-term temperature trends by climate region, 1948 to 2017
| Annual temperature trend, 1948 to 2016 | Summer temperature trend, 1948 to 2016 | Winter temperature trend, 1948 to 2017 | Forest area, 2006 | |
|---|---|---|---|---|
| degrees Celsius | km2 | |||
| Canada | 1.7 | 1.5 | 3.4 | 3,475,757 |
| Arctic Mountains and Fiords | 1.7 | 1.2 | 2.5 | 576 |
| Arctic Tundra | 2.2 | 1.7 | 3.3 | 46,026 |
| Atlantic Canada | 0.7 | 1.3 | 0.6 | 173,370 |
| Great Lakes and St. Lawrence | 0.9 | 1.1 | 1.3 | 92,359 |
| Mackenzie District | 2.7 | 1.9 | 5.0 | 388,751 |
| Northeastern Forest | 1.0 | 1.3 | 2.0 | 1,317,441 |
| Northwestern Forest | 2.1 | 1.6 | 4.3 | 738,947 |
| Pacific Coast | 1.6 | 1.5 | 2.0 | 66,752 |
| Prairies | 1.9 | 0.9 | 3.6 | 71,292 |
| South British Columbia Mountains | 2.0 | 1.5 | 3.0 | 318,113 |
| Yukon and North British Columbia Mountains | 2.6 | 1.3 | 5.7 | 262,130 |
|
Notes: The long-term temperature trend refers to the linear trend in temperature departures from the 1961 to 1990 climate normal over the period of 1948 to 2017. Positive values indicate that temperatures have warmed. Data for forest area are available from the National Forest Inventory by ecozone and have been adjusted to provide climate region totals. Excludes non-inventoried land in the Arctic ecozones (Arctic Cordillera, Northern Arctic, Southern Arctic) and small areas of the Taiga Plains and Hudson Plains ecozones located in Nunavut—areas that are largely devoid of tree cover. Sources: Statistics Canada, Environment, Energy and Transportation Statistics Division, 2018; Environment and Climate Change Canada (ECCC), 2017, "Annual 2016," "Summer 2016," and "Winter 2016-2017," Climate Trends and Variations Bulletin (accessed December 5, 2017); Canada's National Forest Inventory (NFI), 2016, Grouped kNN Map layers (accessed April 7, 2017); NFI, 2013, Table 4.1. Area (1000 ha) of forest and non-forest land by terrestrial ecozone in Canada, 2006 revised baseline, Version 3, December 2013 (accessed April 7, 2017). |
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