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通过对西北太平洋最近九年爆发性气旋的分析表明:气旋的爆发性发展主要发生在冬半年的海洋上,集中在日本东南海域,且有明显的季节性。加深率以1.1贝吉龙居多。其发展过程的云形特征可归为四类:南北逗点云系迭加类;气旋锢囚性发展类;斜压叶状云系类和东西云系迭加类。
Based on the analysis of the explosive cyclone in the past nine years in the western North Pacific, the explosive cyclone mainly occurs in the winter half a year in the ocean and is concentrated in the southeastern Japan with obvious seasonal variations. Deepen the rate of 1.1 Bay Ji Long mostly. The cloud features of the development process can be classified into four categories: the North-South comic cloud system superposition class; the development of cyclonic occlusion; the obliquity leaf cloud system and the East-West cloud system superposition class.