Alaska tundra fires accelerate permafrost thaw and flip Arctic-boreal zone into a carbon source
technologyreview.comNew field research in Alaska's Denali National Park shows how tundra wildfires accelerate permafrost thaw and release carbon. Scientists found that a 2013 fire deepened the seasonally thawed layer by up to two feet in the hottest burn areas. This is one of the few studies with pre-fire baseline data from survey grids established in 2001. The broader Arctic picture is concerning. About 40% of the Arctic-boreal zone now emits more carbon than it absorbs, once fires and permafrost loss are included. Abrupt thaw can double expected emissions and offset any gains from Arctic greening. The findings complicate the idea that plant expansion will compensate for soil carbon losses. Researchers stress that outcomes vary by region and fire severity. Some boreal forest burns recover with deciduous trees that store more carbon, while tundra burns like the 2007 Anaktuvuk River fire keep releasing carbon for decades. These direct measurements are essential for improving climate models and carbon accounting.
