冷涡云系的结构可归纳为单纯的冷涡结构和具有锢囚气旋结构两类。
The structure of cold vortex cloud system is catalogued by two types, the simple vortex structure and the occluded cyclone structure.
利用原始方程模式探讨了高空西风急流和低空南风急流中锢囚锋环流的演变和增强机制。
The evolution and enhancement of occluded frontal circulation in upper-level westerly jet and lower-level southerly jet are discussed by using a dry primitive equation model.
当极地槽和主要的极锋相互作用，会产生不同的过程，会引起短暂的锢囚。
A different process occurs when there is interaction between a polar trough and the main polar front, giving rise to an instant occlusion.
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