Fig. 13From: Impact of the Kuroshio large meander on local atmospheric circulation and precipitation in winterAs for Fig. 9, but showing the difference in specific humidity (color; g kg−1) and the mean wind (vector) at 900 hPa. Solid and dashed contours indicate the SST difference of + 0.5 °C and − 0.5 °C, respectively, between the LM runs minus NLM runsBack to article page