Fig. 8: Long-term effects of an temperature overshoot on wetland formation and soil methane production.
From: Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios
Differences between simulations initialized with the soil carbon concentrations after (P2100) and before (NoOS) an temperature overshoot that persist under nontransient atmospheric conditions (PACT1.5). Shown are relative differences in annual mean inundated area (blue line, left y-axis) as well as relative differences in the soil methane production (red line, right y-axes).
