We're building it up to burn it down: fire occurrence and fire-related climatic patterns in Brazilian biomes

PeerJ. 2022 Oct 25:10:e14276. doi: 10.7717/peerj.14276. eCollection 2022.

Abstract

Background: Terrestrial biomes in South America are likely to experience a persistent increase in environmental temperature, possibly combined with moisture reduction due to climate change. In addition, natural fire ignition sources, such as lightning, can become more frequent under climate change scenarios since favourable environmental conditions are likely to occur more often. In this sense, changes in the frequency and magnitude of natural fires can impose novel stressors on different ecosystems according to their adaptation to fires. By focusing on Brazilian biomes, we use an innovative combination of techniques to quantify fire persistence and occurrence patterns over time and evaluate climate risk by considering key fire-related climatic characteristics. Then, we tested four major hypotheses considering the overall characteristics of fire-dependent, fire-independent, and fire-sensitive biomes concerning (1) fire persistence over time; (2) the relationship between climate and fire occurrence; (3) future predictions of climate change and its potential impacts on fire occurrence; and (4) climate risk faced by biomes.

Methods: We performed a Detrended Fluctuation Analysis to test whether fires in Brazilian biomes are persistent over time. We considered four bioclimatic variables whose links to fire frequency and intensity are well-established to assess the relationship between climate and fire occurrence by confronting these climate predictors with a fire occurrence dataset through correlative models. To assess climate risk, we calculated the climate hazard, sensitivity, resilience, and vulnerability of Brazilian biomes, and then we multiplied the Biomes' vulnerability index by the hazards.

Results: Our results indicate a persistent behaviour of fires in all Brazilian biomes at almost the same rates, which could represent human-induced patterns of fire persistence. We also corroborated our second hypothesis by showing that most fire-dependent biomes presented high thermal suitability to fire, while the fire-independent biome presented intermediate suitability and fire-sensitive biomes are the least suitable for fire occurrence. The third hypothesis was partially corroborated since fire-dependent and independent biomes are likely to increase their thermal suitability to fire, while fire-sensitive biomes are likely to present stable-to-decreasing thermal suitability in the future. Finally, our fourth hypothesis was partially corroborated since most fire-dependent biomes presented low climate risk, while the fire-independent biome presented a high risk and the fire-sensitive biomes presented opposite trends. In summary, while the patterns of fire persistence and fire occurrence over time are more likely to be related to human-induced fires, key drivers of burned areas are likely to be intensified across Brazilian biomes in the future, potentially increasing the magnitude of the fires and harming the biomes' integrity.

Keywords: Climate hazard; Climate risk; Fire persistence; Resilience; Sensitivity index; Vulnerability; Wildfires.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Brazil / epidemiology
  • Ecosystem*
  • Humans
  • Temperature
  • Time Factors

Grants and funding

This study was financed by the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - Brasil (CAPES) - Finance Code 001. Paulo Ferreira received financial support from Fundação para a Ciência e a Tecnologia (grants UIDB/05064/2020 and UIDB/04007/2020). Mariana M. Vale was funded by the Conselho Nacional do Desenvolvimento Científico e Tecnológico (CNPq) (Grant no. 304309/2018-4) and Fundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de Janeiro (FAPERJ) (Grant no. E-26/202.647/2019) and had the support of the National Institute for Science and Technology in Ecology, Evolution and Biodiversity Conservation (CNPq Grant no. 465610/2014-5 and FAPEG Grant no. 201810267000023). Carlos Frederico Duarte Rocha was supported by FAPERJ through the program Cientistas do Nosso Estado (process E-26/202.803/2018) and from CNPq (Processes 302974/2015-6, 424473/2016 and 304375/2020-9), and by Programa Prociência from the Universidade do Estado do Rio de Janeiro (UERJ). Lilian Sales was supported by the Canadian Government through a Banting Postdoctoral Fellowship (FRN 174541). Paulo Ferreira was funded by the National Council for Research and Development (CNPq) (311103/2015-4), Foundation for the Support of Research of the State of Amazonas (FAPEAM) (01.02.016301.000289/2021-33), and National Institute for Research in Amazonia (INPA) (PRJ15.125). Mariana M. Vale and Paulo Ferreira developed this work in the context of the Brazilian Research Network on Climate Change (Rede Clima) (FINEP Grant no. 01.13.0353-00). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.