Table 1.
RF due to Δ[CO2]a (W m−2) | RF due to Δalbedo (W m−2) | RF due to Δ SLCFs (W m-2) | Combined RF due to CO2 (after 100 years), albedo and SLCFs (W m-2) | |
---|---|---|---|---|
Boreal deforestation | 0.01 | −0.51 | 0.01 | −0.49 |
Temperate deforestation | 0.71 | −0.27 | 0.05 | 0.49 |
Tropical deforestation | 1.26 | −0.18 | 0.03 | 1.11 |
Global deforestation | 2.22 | −0.96 | 0.12 | 1.38 |
RCP8.5 level deforestation in 2100 | 0.24b | 0.02b | 0.00 | 0.26 |
Global annual mean radiative forcings (W m−2) due to change to CO2 concentration, albedo and SLCFs, and the net RF due to CO2, albedo and SLCF changes, for each deforestation scenario
aFor idealised deforestation scenarios, CO2 RF is diagnosed 100 years after the initial deforestation
bRF for CO2 and albedo change due to land-use change under RCP 8.5 taken from ref.24