Anthropogenic climate change impacts exacerbate summer forest fires in California

Author:

Turco Marco1ORCID,Abatzoglou John T.2ORCID,Herrera Sixto3ORCID,Zhuang Yizhou4ORCID,Jerez Sonia1ORCID,Lucas Donald D.5ORCID,AghaKouchak Amir67ORCID,Cvijanovic Ivana8

Affiliation:

1. Department of Physics, Regional Atmospheric Modelling Group, Regional Campus of International Excellence Campus Mare Nostrum, University of Murcia, Murcia 30100, Spain

2. Management of Complex Systems Department, University of California, Merced, CA 95343

3. Applied Mathematics and Computer Science Department, University of Cantabria, Santander 39005, Spain

4. Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA 90095

5. National Atmospheric Release Advisory Center, Lawrence Livermore National Laboratory, Livermore, CA 94550-9698

6. Department of Civil and Environmental Engineering, University of California, Irvine, CA 92697

7. Department of Earth System Science, University of California, Irvine, CA 92697

8. ISGlobal–Barcelona Institute for Global Health, Barcelona 08003, Spain

Abstract

Record-breaking summer forest fires have become a regular occurrence in California. Observations indicate a fivefold increase in summer burned area (BA) in forests in northern and central California during 1996 to 2021 relative to 1971 to 1995. While the higher temperature and increased dryness have been suggested to be the leading causes of increased BA, the extent to which BA changes are due to natural variability or anthropogenic climate change remains unresolved. Here, we develop a climate-driven model of summer BA evolution in California and combine it with natural-only and historical climate simulations to assess the importance of anthropogenic climate change on increased BA. Our results indicate that nearly all the observed increase in BA is due to anthropogenic climate change as historical model simulations accounting for anthropogenic forcing yield 172% (range 84 to 310%) more area burned than simulations with natural forcing only. We detect the signal of combined historical forcing on the observed BA emerging in 2001 with no detectable influence of the natural forcing alone. In addition, even when considering fuel limitations from fire-fuel feedbacks, a 3 to 52% increase in BA relative to the last decades is expected in the next decades (2031 to 2050), highlighting the need for proactive adaptations.

Funder

Spanish ministry of Science, Innovation and Universities

MCIN/AEI

La Caixa Junior Leader Grant 2020

Spanish Ministry of Science, Innovation and Universities

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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