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. 2015 Mar 2;112(11):3257–3262. doi: 10.1073/pnas.1423439112

Fig. 2.

Fig. 2.

Same as Fig. 1 but for changes in precipitation (mm/d). (A) Global, (B) Boreal, (C) Temperate, and (D) Tropical. Shading in line plots represents the ±1 SD estimated from the control simulation. Comparison of B with D clearly indicates that the remote effect has a larger influence on tropical precipitation than the local effect. The location of the precipitation centroid in the ITCZ region in the CTL case and the shifts in the experiments are shown above the panels.