Fig. 2 | Nature Communications

Fig. 2

From: Quantifying climate feedbacks in polar regions

Fig. 2

Nonlinearity in the surface albedo feedback factor for three consecutive doublings of CO2. The feedback factor, defined as the ratio of the magnitude of the albedo feedback on the Planck feedback, is calculated using the radiative kernel technique85 and zonal averages are plotted for three consecutive doublings of CO2 concentrations in CCSM3. The global average feedback factor decreases87 from 0.097 for 2xCO2–CNTL to 0.053 for 8xCO2–4xCO2

Back to article page