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Canopy-mediated climate feedbacks in the boreal continuous permafrost zone
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DOI：10.1038/s41558-026-02692-z.png)
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Abstract
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Boreal forests, covering approximately a quarter of the continuous permafrost zone, store relatively modest aboveground carbon, but thermally protect vast soil organic carbon (SOC) pools. Here, using a process-based model to compare seasonal thaw depths under forested and bare-ground scenarios, we quantify distinct canopy thermal insulation capacities of deciduous needleleaf, evergreen needleleaf and deciduous broadleaf canopies on permafrost thermal dynamics. Canopy buffering maintains approximately 59 Pg of carbon in a frozen state, which equals 32% of the total forested permafrost carbon pool and far exceeds boreal biomass stocks (7–19 Pg). Canopy changes could mobilize this frozen SOC through gradual thaw (40 Pg) and rapid thermokarst collapse (19 Pg). While forest loss sacrifices biomass carbon stocks, resulting thaw would expose orders of magnitude more SOC from previously frozen reservoirs, revealing a critical asymmetry. Forest conservation strategies in continuous permafrost zones must account for canopy-mediated thermal protection of frozen SOC, which far exceeds its biomass carbon sequestration capacity. Soil carbon stocks are greater than biomass carbon in boreal forests. This study shows that tree canopies thermally protect more carbon in permafrost from thaw than is stored in biomass, highlighting the need to consider carbon impacts of forest disturbance and conservation on an ecosystem scale.
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