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. 2022 Jan 26;8(4):eabl8278. doi: 10.1126/sciadv.abl8278

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Fig. 2. — Nonzonal component of 200-hPa geopotential height (in m) anomalies in the winter (DJFM) of (A and B) 1982/1983, (C and D) 1997/1998, and (E and F) 2015/2016, for the (A, C, and E) ERA5 reanalysis and (B, D, and F) CESM2 experiment ensemble mean. For the CESM2 experiment, statistically significant values (P < 0.05) are stippled.