南亚高压与西太平洋副热带高压的上下叠加是引起高温天气最主要的环流特征；
The main circulation characteristic of the high temperature weather was the addition of the South Asia high and the Northwest Pacific subtropical high.
中平流层环流转型与对流层重要系统(极涡、西太平洋副热带高压)存在一定关系。
The relation between the transition dates in middle stratosphere and the important systems in troposphere such as polar vortex and the subtropical high in West Pacific.
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