The areal pattern of burned tree vegetation in the subarctic region of northwestern Canada

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Abstract

In terms of its lower areal extent of burns, and lower frequency of air photos showing burns, the forest-tundra is distinct from both open crown and closed crown forest regions. Burns show a general decrease in areal coverage from NW (Mackenzie River to Great Bear Lake: 0-50% of the terrain) to SE (Great Slave Lake to Hudson Bay: 0-10%). In the NW, the flat till plains, high cover of continuous mature forest, and scarcity of lakes, coupled with dominance of slowly regenerating white spruce Picea glauca (in the forest-tundra) may help to account for the extensive burned vegetation. In the E half of the study region, the northern limit of burns normally does not extend beyond the line where tree cover equals upland tundra cover. In this E sub-region, tree cover decreases rapidly northward within the southern half of the forest-tundra, constraining the areal extent of individual burns. -from Authors

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Timoney, K. P., & Wein, R. W. (1991). The areal pattern of burned tree vegetation in the subarctic region of northwestern Canada. Arctic, 44(3), 223–230. https://doi.org/10.14430/arctic1542

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