Table 2 Overview of the simulations that were performed for this study.
From: Timescales of the permafrost carbon cycle and legacy effects of temperature overshoot scenarios
Simulation | Temp. cover | Spatial cover | Forcing | Cinit | Pinit | Sec. | Fig. |
|---|---|---|---|---|---|---|---|
NoOS | 1850–2035 | 45–90°N | Historical + SSP5-8.5 | Observ. | pi-control | 2*1 | |
P2050 | 2035–2065 | 45–90°N | Overshoot, SSP5-8.5 peak in 2050 | NoOS | NoOS | 2*1 | |
P2075 | 2035–2115 | 45–90°N | Overshoot, SSP5-8.5 peak in 2075 | NoOS | NoOS | 2*1 | |
P2100 | 2035–2165 | 45–90°N | Overshoot, SSP5-8.5 peak in 2100 | NoOS | NoOS | 2*1 | |
CC \({}_{{{{\rm{NoOS}}}}}^{{{{\rm{NoOS}}}}}\) | 1000 years | 45–90°N | *3PACT1.5 (SSP5-8.5: 2030–2040) | NoOS | NoOS | 2*1 | |
CC \({}_{{{{\rm{P2050}}}}}^{{{{\rm{P2050}}}}}\) | 1000 years | 45–90°N | *3PACT1.5 (SSP5-8.5: 2030–2040) | P2050 | P2050 | 2*1 | |
CC \({}_{{{{\rm{P2075}}}}}^{{{{\rm{P2075}}}}}\) | 1000 years | 45–90°N | *3PACT1.5 (SSP5-8.5: 2030–2040) | P2075 | P2075 | 2*1 | |
CC \({}_{{{{\rm{P2100}}}}}^{{{{\rm{P2100}}}}}\) | 1000 years | 45–90°N | *3PACT1.5 (SSP5-8.5: 2030–2040) | P2100 | P2100 | 2*1 | |
CC \({}_{{{{\rm{NoOS}}}}}^{{{{\rm{NoOS}}}}}\) | 2500 years | 45–90°N | *4PACT1.5 (SSP5-8.5: 2030–2040) | NoOS | NoOS | 2*2 | |
CC \({}_{{{{\rm{NoOS}}}}}^{{{{\rm{P2100}}}}}\) | 2500 years | 45–90°N | *4PACT1.5 (SSP5-8.5: 2030–2040) | P2100 | NoOS | 2*2 | |
CC-REG\({}_{{{{\rm{NoOS}}}}}^{{{{\rm{NoOS}}}}}\) | 7500 years | Grid box | *4PACT1.5 (SSP5-8.5: 2030–2040) | CC \({}_{{{{\rm{NoOS}}}}}^{{{{\rm{NoOS}}}}}\) | CC \({}_{{{{\rm{NoOS}}}}}^{{{{\rm{NoOS}}}}}\) | 2*2 | |
CC-REG\({}_{{{{\rm{NoOS}}}}}^{{{{\rm{P2100}}}}}\) | 7500 years | Grid box | *4PACT1.5 (SSP5-8.5: 2030–2040) | CC\({}_{{{{\rm{NoOS}}}}}^{{{{\rm{P2100}}}}}\) | CC\({}_{{{{\rm{NoOS}}}}}^{{{{\rm{P2100}}}}}\) | 2*2 |