Fig. 6
From: Impact of the Kuroshio large meander on local atmospheric circulation and precipitation in winter
a Regression coefficients of upward pressure velocity along 138°E based on the ERA5 dataset onto the Kuroshio large meander index from 1982 to 2019. The contour interval is 0.005 Pa s−1. b Difference of the vertical velocity of the model along 138°E between the LM runs minus the NLM runs. The contour interval is 0.2 cm s−1. In a, b, gray shading indicates regions where the corresponding correlation coefficients and the difference are statistically significant at the 95% confidence level, respectively