Fig. 8From: Impact of the Kuroshio large meander on local atmospheric circulation and precipitation in winterAs for Fig. 7, but for the regression coefficients of the 10-m wind as derived from the ERA5 dataset onto the SST of the OISST dataset averaged a over the region indicated by the blue box in Fig. 7 and b over the region indicated by the red box in Fig. 7. The sign of the vectors of b is reversed for ease of comparisonBack to article page