Fig. 1: RICE glacial records between 40 and 26 ka BP.
From: Antarctic evidence for an abrupt northward shift of the Southern Hemisphere westerlies at 32 ka BP

a nssCa2+ 20, b ssNa+ (this study), c δD19. Antarctic Isotope Maxima (AIM) events identified in RICE δD are shown in gray bars and are numbered at the bottom. Downward arrows in nssCa2+ indicate the lowering of concentration during AIM events and arrows pointing upwards in ssNa+ indicate an increase in concentration during AIM events. Black bold lines indicate the timing and magnitude of the mean shift. Thick brown and redline indicate a 50-yr average of the original nssCa2+ and Na+ data, respectively. δD is sampled on a 50-yr interval and smoothed using a 500-yr low pass filter. The latitudinal position of Southern Hemisphere Westerly Winds (SHWW) inferred from nssCa2+ concentration is shown using an arrow on the right side adjacent to the nssCa2+ plot. The direction of spatial change in the open-ocean area based on the Na+ level is shown by an arrow on the left side adjacent to Na+ plot. Higher δD values indicate atmospheric warming. Marine isotope stages (MIS) bracketed in this interval are shown using yellow and green bars at the top. The numbering of the events is based on WAIS Divide Ice Core (WDC)31. Source data are provided as a Source Data file.