The albedo of Earth

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Future climate forcing potentially without precedent in the last 420 million years (2017, background): “Given this understanding, and that summarized in equation (1), the climatic evolution of the Earth over geological time is largely a function of the concentration of the non-condensing greenhouse gases, planetary albedo (A) and the TSI (Fs; for example, ref.”
The Max Planck Institute Grand Ensemble: Enabling the Exploration of Climate System Variability (2019, result): “While a previous study claims that climate models do not represent the variability of these fluxes well (Stephens et al., 2015), Figure 3 shows that the observations are within the model spread, and hence, the model is consistent with observations.”