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AGU: Global Biogeochemical Cycles

 

Keywords

  • forest fires
  • climate change
  • deforestation

Index Terms

  • Global Change: Land cover change
  • Geographic Location: South America
  • Global Change: Impacts of global change
  • Global Change: Biogeochemical cycles, processes, and modeling

Abstract

GLOBAL BIOGEOCHEMICAL CYCLES, VOL. 22, GB4007, 10 PP., 2008
doi:10.1029/2007GB003166

Fire risk in Amazonia due to climate change in the HadCM3 climate model: Potential interactions with deforestation

Nicola Golding

Met Office Hadley Centre, Climate Research, Exeter, UK

Richard Betts

Met Office Hadley Centre, Climate Research, Exeter, UK

Deforestation in Amazonia seems likely to continue in the 21st century, and fire risk could increase as a result of global climate change. With deforestation activities providing a source of ignition, the combination of this with increased fire risk could lead to widespread impacts on Amazonian ecosystems. This would also contribute further to climate change through feedbacks on the global carbon cycle. This study uses the McArthur Forest Fire Danger Index and an ensemble of variants of the HadCM3 climate model to simulate potential changes to fire risk in Amazonia over the 21st century. Significant increases in central and eastern Amazonia are simulated by 2020, and high fire danger for over 50% of the forest is simulated in all model runs by 2080. By 2080, as much as 25% of Amazonia shows high levels of agreement in projections of combined fire risk and deforestation. The areas simulated with high fire danger are also those projected to be impacted most significantly by deforestation. If the regional climate changes simulated for Amazonia by HadCM3 are realistic, the risk of significant forest damage could become high, and deforestation activities could, therefore, have a greater potential for impacting on wider areas of forest.

Received 10 December 2007; accepted 25 June 2008; published 11 November 2008.

Citation: Golding, N., and R. Betts (2008), Fire risk in Amazonia due to climate change in the HadCM3 climate model: Potential interactions with deforestation, Global Biogeochem. Cycles, 22, GB4007, doi:10.1029/2007GB003166.

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