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. 2019 Oct 30;5(10):eaax1697. doi: 10.1126/sciadv.aax1697

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Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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Fig. 2 — Wettest month 500-mbar geopotential height (isolines), wind field (black arrows), and precipitation in the Hauterivian (A), Santonian (B), and Zanclean (C) (paleo-rotated region in blue line). Wettest month zonal cross-sectional (0°N to 60°N, 105°E to 112.5°E) vertical velocity in the Hauterivian (D), Santonian (E), and Zanclean (F) depicting the position of the Hadley circulation; negative values indicate vertical ascent, positive values indicate vertical descent, and vertical black lines depict maximum and minimum latitudinal extent of rotated EAM region. Mean annual meridional (10°S to 10°N) depth profile ocean temperature (°C) for the Hauterivian (G), Santonian (H), and Zanclean (I) depicting the location of the Pacific warm pool. Red circles denote region of interest highlighted in the main text.