Polar vortex is a basic circulation system which exists in every season (strong in winter and weak in summer) and can extend to the lower level of stratosphere.
极涡是该区域四季存在、冬强夏弱、向上延伸至平流层下部的基本环流系统。
The mechanisms coupling the stratosphere and troposphere have been studied by some scientists for understanding the effect of the polar vortex change on the lower circulation.
一些学者已通过平流层和对流层耦合机制的研究探索极涡变化对低层环流的作用。
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