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Global burned area increasingly explained by climate change

  • Chantelle Burton,
  • Seppe Lampe,
  • Douglas I. Kelley,
  • Wim Thiery,
  • Stijn Hantson,
  • Nikos Christidis,
  • Lukas Gudmundsson,
  • Matthew Forrest,
  • Eleanor Burke,
  • Jinfeng Chang,
  • Huilin Huang,
  • Akihiko Ito,
  • Sian Kou-Giesbrecht,
  • Gitta Lasslop,
  • Wei Li,
  • Lars Nieradzik,
  • Fang Li,
  • Yang Chen,
  • James Randerson,
  • Christopher P. O. Reyer,
  • Matthias Mengel

摘要

Fire behaviour is changing in many regions worldwide. However, nonlinear interactions between fire weather, fuel, land use, management and ignitions have impeded formal attribution of global burned area changes. Here, we demonstrate that climate change increasingly explains regional burned area patterns, using an ensemble of global fire models. The simulations show that climate change increased global burned area by 15.8% (95% confidence interval (CI) [13.1–18.7]) for 2003–2019 and increased the probability of experiencing months with above-average global burned area by 22% (95% CI [18–26]). In contrast, other human forcings contributed to lowering burned area by 19.1% (95% CI [21.9–15.8]) over the same period. Moreover, the contribution of climate change to burned area increased by 0.22% (95% CI [0.22–0.24]) per year globally, with the largest increase in central Australia. Our results highlight the importance of immediate, drastic and sustained GHG emission reductions along with landscape and fire management strategies to stabilize fire impacts on lives, livelihoods and ecosystems.