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Arctic 'zombie fires' rising from the dead could unleash vicious cycle of warming




So-called "zombie fires" in the peatlands of Alaska, Canada and Siberia disappear from the Earth's surface and smoulder underground during the winter before coming back to life the following spring. These fires puzzle scientists because they appear in early May, way ahead of the usual fire season in the far north, and can reignite for a number of years.

Most scientists believe that zombie fires are the remnants of fires on the surface, but we have identified an alternative cause. Our research suggests that rapid atmospheric warming above ground can cause peat soils to suddenly heat up to smouldering temperatures underground, all without any spark or other ignition. These zombie fires may be a case of climate change-driven spontaneous combustion.

Reports of such fires date back to 1940s, when they were rare events. However, the frequency and intensity of these fires has increased significantly in the past two decades, hand in hand with accelerated warming in the Arctic, the fastest-warming region on the planet.

At the start of 2024, more than 100 zombie fires were active in the Canadian province of British Columbia alone. Zombie fires have even been recorded near the coldest village on earth, Oymyakon in north eastern Siberia, where they carried over through multiple winters and account for around 3.5% of area burned in the wider region each year.

world map showing carbon-rich peat soils.

Red areas are warming fastest, while black and grey areas show carbon-rich peat soils. There is significant overlap between the two, such as in Cherskii in northern Siberia. (Image credit: O'Sullivan et al / Royal Society A (Data: Berkeley Earth / PEATMAP))

More carbon is trapped in temperature-sensitive Arctic peat soils than is found in the entire atmosphere, and these fires are releasing gigatonnes of it into the atmosphere. We wanted to know if sudden warming might be directly responsible.

Two remarkable results

We developed a mathematical model to explore different what-if scenarios, including how the temperature and carbon content of peat soils respond to changes in the weather and climate. Crucially, our model captures how certain microbes generate heat while breaking down soil and releasing its carbon into the atmosphere.

We obtained two remarkable results: