Fig. 7: Simulated rain amounts in western Cuba. | Communications Earth & Environment

Fig. 7: Simulated rain amounts in western Cuba.

From: Hydroclimate variability in the northern Caribbean during the last deglaciation was modulated by large-scale atmospheric circulation and climate events

Fig. 7

A During the interval of interest covered by our record from TraCE-21K-II, the CCSM3-based transient all-forcing paleoclimate simulation84. The model supports the overall millennial-scale variations seen in our record. The highlighted green and brown boxes (A) are shown in (B, C), respectively, as regional rainfall trends during the (B) B/A and (C) early deglaciation periods.

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