Fig. 3: Winter mixed layer depth (MLD) and meridional overturning stream function. | Communications Earth & Environment

Fig. 3: Winter mixed layer depth (MLD) and meridional overturning stream function.

From: Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection

Fig. 3

a MLD during austral winter (June to August) in PI, (b) LIG and (c) LIG-PI, and (d) global stream function in PI, (e) LIG and (f) LIG-PI. A paleo-calendar adjustment is applied to the LIG data in (b) and (c) such that its months have the same angular definition as PI as described in Bartlein and Shafer68.

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