The Kuroshio and Gulf regions are two hugest marine heating sources in the mid-latitude, the anomaly heating from these two regions has very important effects on the atmospheric circulation of the North Hemisphere. In this study,the relationship of the marine anomaly heating in the Kuroshio and Gulf regions in winter to the Subtropical High and the westerlies circulation in mid-high latitude in summer are analyzed, the physical processes are discussed. The results show that when the winter monsoon in East Asia and in North America is stronger(weaker), the Subtropical High and Ural and Okhotsk High will be weaker(stronger) in summer,which variations form a drought(flood )circulation pattern for the middle and the lower reaches of Changjiang River.