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Updated: May 9, 2026

Simulating Impacts of Ice Storms on Forest Ecosystems
06:27

Simulating Impacts of Ice Storms on Forest Ecosystems

Published on: June 30, 2020

Fire regime zonation under current and future climate over eastern Canada.

Yan Boulanger1, Sylvie Gauthier, David R Gray

  • 1Natural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, 1055 du P.E.P.S., P.O. Box 10380, Station Sainte-Foy, Quebec, Quebec G1V 4C7, Canada. yan.boulanger@nrcan.gc.ca

Ecological Applications : a Publication of the Ecological Society of America
|July 20, 2013
PubMed
Summary
This summary is machine-generated.

Climate change will significantly alter Canadian forest fire regimes, increasing fire frequency and area burned. Homogeneous Fire Regime (HFR) zones help predict these changes for better forest management.

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Area of Science:

  • Forestry and Ecology
  • Climate Science
  • Fire Ecology

Background:

  • Forest fires are a major disturbance in Canadian ecosystems, significantly influenced by climate.
  • Understanding fire regimes is crucial for biodiversity, carbon cycling, and forest management.
  • Projected climate change necessitates defining homogeneous fire regime (HFR) zones to predict future impacts.

Purpose of the Study:

  • To delineate current and future homogeneous fire regime (HFR) zones in eastern Canada.
  • To model the relationship between historical fire regime attributes and climatic/environmental variables.
  • To project how fire regimes will change under future climate scenarios.

Main Methods:

  • Utilized Random Forests (RF) modeling to analyze fire regime attributes (1961-1990).
  • Employed climatic normals from the Canadian Regional Climate Model (CRCM) for current and future projections.
  • Delineated HFR zones for multiple future time periods (2011-2100).

Main Results:

  • Projected heterogeneous responses of fire regimes across eastern Canada, with some regions experiencing minor alterations and others significant shifts.
  • Predicted a 2.2-fold increase in fire frequency and a 2.4-fold increase in annual area burned.
  • Anticipated a slight shift in the fire season later into the summer (5-20 days) for many areas due to increased extreme fire-weather and drought codes.

Conclusions:

  • HFR zonation provides critical insights into regional fire regime variations under climate change.
  • Identified specific zones with unique fire regime responses, which would be obscured by broader administrative or ecological stratifications.
  • The findings are valuable for informing adaptive forest and fire management strategies in Canada.