The Anomaly Change of Subtropical High and Its Formation Cause in West Pacific
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Abstract:
The anomalous climatic characteristics of subtropical high and its formation cause in the West Pacific in 1994 is analysed. It is shown that the intensity is strong,the seasonal northward jump is earlier than normal and the position is persistenly further north in midsummer. Such characteristics associate with the ocean-atmosphere interaction besides the climatic backgrounds.Meanwhile, the SST anomaly field responded to the subtropical high anomaly is discussed.