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. 2019 Jun 5;5(6):eaav3809. doi: 10.1126/sciadv.aav3809

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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. 4 — Similar temperature reconstructions between the Greenland, Mediterranean Sea, and central Europe areas (A) that show a different early to middle Holocene trend compared to high-latitude proxies and model simulations (B). (A) Switzerland MC-FIT (black; this study), Mediterranean SST (23) (pink) (both smoothed with a seven-value running mean) and Greenland GISP2 temperature (10) (blue; 401 years running mean) are shown together with July insolation at 30°N (51)(gray) and LIS sea level rise rate (33) (red). (B) European pollen record (4) (green) and Eurasia δ¹⁸O_c (as winter temperature indicator) (5) (yellow). Also shown are Switzerland MC-FIT (black), regional CCSM3 (3) (orange), and mid-latitude band (30° to 60°N) LOVECLIM (10) (blue) transient simulations of mean annual temperatures. Anomalies are shifted for comparison.