Fig. 5
From: Impact of the Kuroshio large meander on local atmospheric circulation and precipitation in winter
Difference of a 10-m wind and b the corresponding divergence over the ocean between the LM runs minus NLM runs. In a, the black (gray) vectors indicate the regions where the difference of zonal or (and) meridional wind is (not) statistically significant at the 95% confidence level. Red and blue contours indicate the SST difference of + 0.5 °C and–0.5 °C, respectively, between the LM runs minus NLM runs (see Fig. 2). In b, the contour indicates the regions where the difference is statistically significant at the 95% confidence level