Editing Severe wildfire exposes remnant peat carbon stocks to increased post-fire drying

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BTLWS: Bridge To Land Water Sky
CCRN: Changing Cold Regions Network
CRHO: The Canadian Rockies Hydrological Observatory
DRI: Drought Research Initiative
GWF: Global Water Futures
GWFO: Global Water Futures Observatories
INARCH: International Network of Alpine Research Catchment Hydrology
IP3: Improving Processes & Parameterization for Prediction in Cold Regions Hydrology
MAGS: The Mackenzie Global Energy and Water Cycle Experiment (GEWEX) Study

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Abstract

The potential of high severity wildfires to increase global terrestrial carbon emissions and exacerbate future climatic warming is of international concern. Nowhere is this more prevalent than within high latitude regions where peatlands have, over millennia, accumulated legacy carbon stocks comparable to all human CO2 emissions since the beginning of the industrial revolution. Drying increases rates of peat decomposition and associated atmospheric and aquatic carbon emissions. The degree to which severe wildfires enhance drying under future climates and induce instability in peatland ecological communities and carbon stocks is unknown. Here we show that high burn severities increased post-fire evapotranspiration by 410% within a feather moss peatland by burning through the protective capping layer that restricts evaporative drying in response to low severity burns. High burn severities projected under future climates will therefore leave peatlands that dominate dry sub-humid regions across the boreal, on the edge of their climatic envelopes, more vulnerable to intense post-fire drying, inducing high rates of carbon loss to the atmosphere that amplify the direct combustion emissions.

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