Evolution of the global surface temperature of the last 22 ka: the reconstructions of M13 (1) (blue) after 11.3 ka and by Shakun et al. Evolution of the.

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Evolution of the global surface temperature of the last 22 ka: the reconstructions of M13 (1) (blue) after 11.3 ka and by Shakun et al. Evolution of the global surface temperature of the last 22 ka: the reconstructions of M13 (1) (blue) after 11.3 ka and by Shakun et al. (11) (cyan) before 6.5 ka, the model annual mean temperature averaged over the global grid points (black), and the model seasonally biased temperature averaged over the proxy sites (red). The models are the CCSM3 (7), FAMOUS (8), and LOVECLIM (9), with the ensemble mean shown by heavy solid lines and individual members shown by light thin lines [the LOVECLIM (○) and FAMOUS (□) are marked]. Each temperature curve is aligned at 1 ka. The ensemble mean model annual temperature averaged over proxy sites is also shown (yellow, individual models for the Holocene in Fig. 3), whose similarity to the model grid average demonstrates the insensitivity of the temperature trend to the average scheme. (Inset) Expanded part after 2 ka, with the addition of the last millennium experiment in the CCSM4 (gray), which is forced additionally by volcanic aerosol and solar variability (10). ann, annual. Zhengyu Liu et al. PNAS 2014;111:34:E3501-E3505 ©2014 by National Academy of Sciences