A wildfire burn site near the University of Alaska Fairbanks is now teaching researchers how fires accelerate permafrost thaw by stripping insulating soils, risking major carbon releases.
In July 2021, during an unusually hot stretch in interior Alaska, a wildfire broke out on the northern edge of the University of Alaska Fairbanks campus. The fire—likely triggered by lightning—moved quickly through the boreal forest, feeding on a dry layer of feather mosses and lichen before surging into the treetops of black spruce and paper birch. By the time crews arrived, flames were reported at roughly 12 feet high, pushing a smoke plume about 500 feet into the sky.
Nearly five years after that event, the burn area has become a field classroom. In 2024, the Alaska Fire Science Consortium—an organization that briefs wildfire managers on new research—helped establish an educational walking route through the site, placing interpretive signs along cross-country ski trails where field horsetail grows thick along the path. About half a mile in, the forest opens into a stark patch of standing, charred trunks, their needles gone and the surrounding vegetation stripped away.
There, consortium coordinator Hilary Shook demonstrated a simple but telling measurement: a thaw probe, a T-handled steel rod used to find the top of permafrost, the long-frozen layer beneath the surface. Permafrost underlies around 15% of land across the Northern Hemisphere and holds an immense carbon reserve—about twice as much as is currently in the atmosphere.
Just outside the burn scar, Shook’s probe met the hard, frozen layer roughly a foot down. Inside the burned zone, where the fire consumed the moss and organic-rich soil that normally insulate the ground, the probe sank at least three times deeper. Alison York, the consortium’s outgoing coordinator, said the shift was visible even soon after the fire. Monitoring showed the ground had already begun to thaw substantially.
That small demonstration points to a much larger and fast-growing concern across the far north. As climate change drives hotter, drier conditions, boreal and Arctic fires are becoming more frequent and intense. Those fires, in turn, speed up permafrost thaw by removing the protective surface layer. Once thawed, previously frozen organic material can decompose, releasing climate-warming gases and setting off a feedback loop: more warming leads to more fire, which leads to more thaw, which releases more greenhouse gases.
The scale of the problem has been underscored by recent fire seasons. In 2023, Canada’s fires emitted more carbon than the country’s fossil fuel emissions combined—an alarming marker of how quickly northern landscapes could shift from absorbing carbon to releasing it.
Fire policy complicates the picture. Across Alaska and Canada, many large blazes burn in remote regions where agencies often allow fires to run their course as long as communities and infrastructure aren’t threatened. But scientists warn that if warming and fire escalation continue, the boreal forest and its underlying permafrost could increasingly transform from a global carbon sink into a major carbon source.
Researchers across the United States, Canada, and beyond are now racing to quantify what’s at risk—economically as well as ecologically—and to test whether intervention could curb emissions. Proposed approaches include prescribed burns to reduce fuel loads, better systems for rapid detection, and aggressive suppression of fires before they become megafires. Some teams are also examining an idea that once seemed out of bounds: dispatching firefighters not primarily to protect homes, but to defend high-carbon permafrost landscapes.
“We need to figure out a better way to live with wildfire,” said Brendan Rogers, a senior scientist at the Woodwell Climate Research Center, who argues that targeted action could have meaningful climate benefits.
Woodwell is joining forces with the University of Victoria’s POLIS Project on Ecological Governance and the nonprofit Alaska Venture Fund on a multimillion-dollar initiative called North Fire. The partnership aims to study these interventions and build public understanding of their potential, according to MIT Technology Review. The effort is ambitious—and contentious—because it challenges long-standing assumptions about where, when, and why societies should fight fire.
Why it matters
The northern fire boom is no longer just a regional emergency: it threatens a vast carbon store that influences the global climate. Decisions about whether to suppress remote fires could affect greenhouse-gas emissions for decades, reshaping priorities for fire agencies and policymakers. What happens next will depend on whether interventions can be shown to work at scale—and whether governments are willing to rethink “let it burn” strategies in a warming Arctic.
