Abstract

Research highlights—Feedbacks between fire severity, vegetation structure and ecosystem flammability are understudied in highly fire-tolerant forests that are dominated by epicormic resprouters. We examined the relationships between the severity of two overlapping fires in a resprouting eucalypt forest and the subsequent effect of fire severity on fuel structure. We found that the likelihood of a canopy fire was the highest in areas that had previously been exposed to a high level of canopy scorch or consumption. Fuel structure was sensitive to the time since the previous canopy fire, but not the number of canopy fires. Background and Objectives—Feedbacks between fire and vegetation may constrain or amplify the effect of climate change on future wildfire behaviour. Such feedbacks have been poorly studied in forests dominated by highly fire-tolerant epicormic resprouters. Here, we conducted a case study based on two overlapping fires within a eucalypt forest that was dominated by epicormic resprouters to examine (1) whether past wildfire severity affects future wildfire severity, and (2) how combinations of understorey fire and canopy fire within reburnt areas affect fuel properties. Materials and Methods—The study focused on ≈77,000 ha of forest in south-eastern Australia that was burnt by a wildfire in 2007 and reburnt in 2013. The study system was dominated by eucalyptus trees that can resprout epicormically following fires that substantially scorch or consume foliage in the canopy layer. We used satellite-derived mapping to assess whether the severity of the 2013 fire was affected by the severity of the 2007 fire. Five levels of fire severity were considered (lowest to highest): unburnt, low canopy scorch, moderate canopy scorch, high canopy scorch and canopy consumption. Field surveys were then used to assess whether combinations of understorey fire (<80% canopy scorch) and canopy fire (>90% canopy consumption) recorded over the 2007 and 2013 fires caused differences in fuel structure. Results—Reburn severity was influenced by antecedent fire severity under severe fire weather, with the likelihood of canopy-consuming fire increasing with increasing antecedent fire severity up to those classes causing a high degree of canopy disturbance (i.e., high canopy scorch or canopy consumption). The increased occurrence of canopy-consuming fire largely came at the expense of the moderate and high canopy scorch classes, suggesting that there was a shift from crown scorch to crown consumption. Antecedent fire severity had little effect on the severity patterns of the 2013 fire under nonsevere fire weather. Areas affected by canopy fire in 2007 and/or 2013 had greater vertical connectivity of fuels than sites that were reburnt by understorey fires, though we found no evidence that repeated canopy fires were having compounding effects on fuel structure. Conclusions—Our case study suggests that exposure to canopy-defoliating fires has the potential to increase the severity of subsequent fires in resprouting eucalypt forests in the short term. We propose that the increased vertical connectivity of fuels caused by resprouting and seedling recruitment were responsible for the elevated fire severity. The effect of antecedent fire severity on reburn severity will likely be constrained by a range of factors, such as fire weather.

Highlights

  • Wildfire size, the annual area burned and the extent of high severity fire are increasing across many forested regions worldwide [1]

  • We address two questions in this study: (1) Are patterns in reburn severity influenced by antecedent fire severity? (2) Has fuel structure changed in response to combinations of canopy fire and understorey fire within areas of reburnt forest? We used remotely sensed measures of wildfire severity to test whether the severity of the 2013 fire was affected by the severity of the 2007 fire

  • Under SEV weather, the likelihood of canopy consumption (CC) was greater in areas that were previously exposed to fires that consumed or scorched most of the canopy foliage (i.e., high canopy scorch (HCS) and CC) relative to areas that were affected by low canopy scorch (LCS) or were unburnt vegetation (UB) (Figure 3)

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Summary

Introduction

The annual area burned and the extent of high severity fire are increasing across many forested regions worldwide [1]. Feedbacks between fire and vegetation have the potential to either constrain or increase the effect of climate on future wildfire behaviour through the modification of fuel properties and ecosystem flammability [11,12]. These feedbacks remain poorly understood [13,14], and as such, are rarely incorporated into projections of the effects of climate change on ecosystem flammability and fire regimes [11]. The flammability of a fuel particle is determined by its physical properties (e.g., size, shape, moisture content and calorific value) and the exogenous conditions under which the fuel ignites and burns [16,17]

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