Fig. 4: The comparisons between the speleothem δ18O records in this study site and other records. | npj Climate and Atmospheric Science

Fig. 4: The comparisons between the speleothem δ18O records in this study site and other records.

From: Dipolar hydroclimate pattern changes in southwest China during the last deglaciation

Fig. 4

A speleothem δ18O (Yingpan Cave, this study, the dark blue thick line indicates the 5-points smoothed averages) and the insolation of July at 65°N (grey curve)71; B speleothem δ18O (Mawmluh Cave)37; C speleothem δ18O (Haozhu Cave)50; D speleothem δ18O (Hulu Cave)6; E 231Pa/230Th and εNd profiles from core GGC5 from the Bermuda Rise, 4541 m51,52, and F Greenland average temperature reconstruction ±1 SD uncertainty53.

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