Fig. 5From: Future projection of greenhouse gas emissions due to permafrost degradation using a simple numerical scheme with a global land surface modelThe cumulative CO2 flux [TgC] (bottom, left) and CH4 flux [TgCH4] (bottom, right) due to the permafrost degradation (dynamic + thermodynamic) at the end of the twenty-first century in the RCP8.5 scenario. The average of all ensemble members is shownBack to article page