Why Is the Influence of Sunspot Peaks on the Ocean and Atmosphere in Northern Winter Seen Mainly in the Pacific Region?
Figure 3
Anomalies of vertical motion in January-February in five recent sunspot peaks: 30N–30S, 125E-125W (Hadley circulation). Anomalies of vertical motion, January-February, in five recent sunspot peaks: 120E–125W, 5N–10S (Walker circulation). Anomalies of zonal wind in five recent sunspot peaks: 10S–5N, 120E–125W.
