Fig. 9
From: Impact of the Kuroshio large meander on local atmospheric circulation and precipitation in winter
Difference in a precipitation, b evaporation and c horizontal moisture convergence over the ocean between the LM minus NLM runs. Solid and dashed 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 a, the gray contours indicate the regions where the corresponding correlation coefficients are statistically significant at the 95% confidence level