Fig. 4From: Interannual variation of the Warm Arctic–Cold Eurasia pattern modulated by Ural blocking and the North Atlantic Oscillation under changing sea ice conditionsWinter circulation and SAT patterns related to reversed winter sea ice change over the BKS. a Regressed observed winter SAT (shading; °C) and SLP (contour; hPa; 0.4 intervals with negative values shown by dashed lines) anomalies on observed winter SIC over the BKS. Note that SIC was sign-reversed and normalized. b, c Similar to (a), but (b) is for the 10-member mean of the high-correlation group, c is for the 10-member mean of the low-correlation group. d The difference between (b) and (c). Dots in a–c denote shading statistically significant at the 0.05 level by Student's t testBack to article page