Abstract

Wildfires and outbreaks of the spruce budworm, Choristoneura fumiferana (Clem.), are the two dominant natural disturbances in Canada’s boreal forest. While both disturbances have specific impacts on forest ecosystems, it is increasingly recognized that their interactions also have the potential for non-linear behavior and long-lasting legacies on forest ecosystems’ structures and functions. Previously, we showed that, in central Canada, fires occurred with a disproportionately higher frequency during a ‘window of opportunity’ following spruce budworm defoliation. In this study, we use Ontario’s spatial databases for large fires and spruce budworm defoliation to locate where these two disturbances likely interacted. Classification tree and Random Forest procedures were then applied to find how spruce budworm defoliation history, climate, and forest conditions best predict the location of such budworm–fire interactions. Results indicate that such interactions likely occurred in areas geographically bound by hardwood content in the south, the prevalence of the three major spruce budworm host species (balsam fir, white spruce and black spruce) in the north, and climate moisture in the west. The occurrence of a spruce budworm–fire interaction inside these boundaries is related to the frequency of spruce budworm defoliation. These patterns provide a means of distinguishing regions where spruce budworm attacks are likely to increase fire risk.

Highlights

  • Two main types of natural disturbances have dominated Canada’s boreal forest: wildfire and outbreaks of spruce budworm (SBW), Choristoneura fumiferana (Clem.) [1,2]

  • Locating Where Spruce Budworm Defoliation Contributed to Fire

  • We began by distinguishing the bioclimatic conditions in the areas of the spruce budworm belt where a ‘likely interaction’ between spruce budworm defoliation and a large fire occurred, from fromthose thoseareas areasofofthe the belt where there no ‘likely interaction’

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Summary

Introduction

Two main types of natural disturbances have dominated Canada’s boreal forest: wildfire and outbreaks of spruce budworm (SBW), Choristoneura fumiferana (Clem.) [1,2]. In the simplest and most direct form of these interactions, a warmer, drier climate is expected to increase the tendency of SBW-killed stands to burn [7] This effect would likely be magnified by the fact that the spatial extent of SBW outbreaks, and the availability of SBW-attacked stands, already much greater than the extent of fires [2], may increase with climate change [5]. When considered together, these factors suggest that in a drier, warmer climate, the boreal forest may experience accelerated carbon releases due to the interaction of SBW and wildfire disturbance regimes. Recent carbon budget studies have shown that climate change-induced modifications of disturbance regimes have critical impacts on the net atmospheric carbon exchange [8,9]

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