Skip to main content
. Author manuscript; available in PMC: 2019 Apr 10.
Published in final edited form as: Nature. 2018 Oct 10;562(7726):259–262. doi: 10.1038/s41586-018-0577-1

Table 1.

Biogeochemical and biophysical effects in 2100 for four different forest management portfolios over Europe. The business as usual simulation which served as a control, was repeated three times with slightly different initial atmospheric conditions (see Methods “Equilibrium climate for the management portfolios”). The variability between these three repetitions was considered the minimal model noise of the climate model. The reported noise was taken to be the definition of one standard deviation. TOA denotes the radiative imbalance at the top of the atmosphere.

Variable name (units) Business as usual (BAU) Maximise carbon sink Maximise albedo Reduce near-surface temperature
Global average TOA (W m-2) 4.31 ± 0.01 4.31 4.33 4.32
Δ2100-2010 CO2 sink & avoided emissions (Pg C) 4.7 12.8 5.0 8.1
Δ2100-2010 net cumulated atmospheric CO2 (Pg C) 2.7 7.0 2.8 4.5
Atmospheric CO2 (ppm) 934.6 932.6 934.6 933.8
Near surface temperature (K) 283.84 ± <0.001 283.84 283.83 283.81
Annual precipitation (mm) 734.7 ± 0.1 732.6 730.0 730.9
Summer precipitation (mm) 166.1 ± 0.1 165.2 163.7 165.0
Wood harvest (Tg C y-1) 203.2 179.5 144.5 151.6
Surface albedo (-) 0.113 ± <0.0001 0.113 0.128 0.126
Evapotranspiration (mm) 555.5 ± 0.1 552.8 546.4 549.2
Latent heat (W m-2) 44.35 ± <0.01 44.13 43.60 43.82
Sensible heat (W m-2) 26.67 ± <0.01 26.82 27.28 27.00
Total cloud cover (%) 46.8 ± <0. 1 46.7 46.7 46.6