Baseline (i.e., mean 1971 — 1999) global varies between 461 Pg C and 998 Pg C, and increases with ΔMLT for all vegetation models under all 110 climate and CO2 increase scenarios (Fig. 1)(see Materials and Methods and
SI Text for details of simulations).
Figure 2.2 Dynamics of the detrended global temperature anomaly (dT) and detrended negative Length of Day -LRB-- LOD)(
see text for details).
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Following a class reading of Extra Yarn, ask students to retell the story, returning to
the text for details that support the main idea.
Fig 2.3 Dynamics of the detrended global temperature anomaly (dT) and the Zonal Atmospheric Circulation Index (zonal ACI)(see
text for details).
Dipole moment predicted by spherical harmonic field models CALS10k.1 b (red), CALS3k.4 (blue), CALS3k.3 (light blue), CALS7K.2 (grey) and by the archeomagnetic VADM reconstructions by Knudsen et al. (2008)(black) and Genevey et al. (2008)(brown) with uncertainty estimates (dashed lines and error bars) as provided by the authors, see
text for details.