Global warming

Geology

Climate change

Organic chemistry

Biology

Boreal

Physical geography

Oceanography

Permafrost

Paleontology

Geography

Active layer

Chemistry

Geotechnical engineering

Ecology

Earth science

Layer (electronics)

Thermokarst

Hydrology (agriculture)

Forestry

Environmental science

Peat

Thin-film transistor

Taiga

Nature Communications

Permafrost vulnerability to climate change may be underestimated unless effects of wildfire are considered. Here we assess impacts of wildfire on soil thermal regime and rate of thermokarst bog expansion resulting from complete permafrost thaw in western Canadian permafrost peatlands. Effects of wildfire on permafrost peatlands last for 30 years and include a warmer and deeper active layer, and spatial expansion of continuously thawed soil layers (taliks). These impacts on the soil thermal regime are associated with a tripled rate of thermokarst bog expansion along permafrost edges. Our results suggest that wildfire is directly responsible for 2200 ± 1500 km

Wildfire as a major driver of recent permafrost thaw in boreal peatlands