Fig. 5: Temperature anomalies and the difference between them. | Nature Geoscience

Fig. 5: Temperature anomalies and the difference between them.

From: A salty deep ocean as a prerequisite for glacial termination

Fig. 5

a,b, Temperature anomalies by AMOC weakening for interglacial (PIDPERT − PIDCTRL) (a) and Last Glacial Maximum (LGMPERT − LGMCTRL) (b) conditions between model years 100 and 200 as a 100 yr mean, zonally averaged in the Atlantic sector. c, The difference between the glacial and interglacial anomalies (LGM − PID). Plotted using Ocean Data View (http://odv.awi.de).

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